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STATE OF FLORIDA
STATE BOARD OF CONSERVATION
Ernest Mitts, Director

FLORIDA GEOLOGICAL SURVEY
Herman Gunter, Director





GEOLOGICAL BULLETIN NO. 37






GEOLOGY OF JACKSON COUNTY, FLORIDA







by
WAYNE E. MOORE
Associate Professor
VIRGINIA POLYTECHNIC INSTITUTE


Published for
THE FLORIDA GEOLOGICAL SURVEY
Tallahassee, 1955




/1"


AGRI-
CULTURAL
LIBRARY


Frontispiece
Aturia alabamensis (Morton), lateral view xO.6. Specimen is from the upper
2-3 feet of the Bumpnose member of the Crystal River formation, locality J-5.
(F.G.S. no. 1-7387).
ii






ABSTRACT
This is a report of a detailed study of the geology of Jackson
County, Florida. As a result of limited testing, certain clays ap-
pear to be suitable for the manufacture of common brick, tile, re-
fractory brick, and art pottery. Abundant high calcium limestone
reserves are available, and these, with the Miocene clays, could be
used to manufacture cement. One localized structure may have
produced a trap for petroleum.
The county can be divided into three physiographic units: the
Marianna River Valley Lowlands, the Delta Plain Highlands, and
the Terraced Coastal Lowlands, all minor units of the Coastal Plain
Province. These minor units have been produced by the degrada-
tion and alluviation of streams and by the coastal erosion of the
sea. Although limestone now crops out at the surface, the Marianna
River Valley Lowlands are the result of normal stream erosion of
the plastic sediments that once mantled the area. Three stream
terraces, a high delta plain, and a marine terrace are to be found
in the county.
Six units of Tertiary rocks are shown on the geological map.
The oldest rock cropping out in the county is the Crystal River
formation. Although the Bumpnose limestone, a new stratigraphic
name, was mapped in detail, it is given a member designation since
it is believed to be a facies of the Crystal River formation. The
shallow water fauna of the Crystal River formation grades downdip
into a deeper water fauna that characterizes the Gadsden limestone,
a new formation. The absence of the Marianna limestone at the
surface in eastern Jackson County is caused by a combination of
structure, erosion, and terrace mantle. The Suwannee limestone
thickens rapidly to the south between Dry Creek and Sink Creek.
Erosion of the Suwannee limestone from structural highs before
the deposition of the overlying Tampa formation is responsible for
this thickening.
The Tampa formation in Jackson County consists predominantly
of plastic deposits to the west and north and is essentially calcareous
to the south and east. No deposits that could be assigned to younger
Miocene formations were recognized in the county, but it is possible
that a part of what is considered to be Tampa formation in this
report may be younger than that formation. In particular, beds in
the southwestern part of the county may belong to Miocene forma-
tions younger than the Tampa formation. The age of the highest
sand deposits in the southwestern part of the county is probably
Pliocene ?-Pleistocene.









FLORIDA STATE BOARD

OF

CONSERVATION


LEROY COLLINS
Governor


R. A. GRAY
Secretary of State



J. EDWIN LARSON
Treasurer


NATHAN MAYO
Commissioner of Agriculture



THOMAS D. BAILEY
Superintendent Public Instructhon


CLARENCE M. GAY
Comptroller


RICHARD ERVIN
Attorney General


ERNEST MITTS
Director of Conservation





LETTER OF TRANSMITTAL


Jlorida geological Survey

Callakassee

March 25, 1955


Honorable Ernest Mitts, Director
Florida State Board of Conservation
Tallahassee, Florida

Sir:

This report, being published as Florida Geological Survey Bul-
letin 37, is entitled THE GEOLOGY OF JACKSON COUNTY,
FLORIDA, and it was prepared by Wayne E. Moore, Associate Pro-
fessor of Geology at Virginia Polytechnic Institute while he was
a candidate for the degree of Doctor of Philosophy at Cornell Uni-
versity. This department supervised the field work, and the faculty
at Cornell University supervised the laboratory work and the prepa-
ration of the manuscript.

As originally submitted the manuscript could not be published
and the details of editing were largely unacceptable to the writer.
In order that the locations of the outcrops and the details of the
economic evaluation can be made available to the public, the report
is being published without additional editing although the reader
should keep in mind that the opinions expressed are those of the
writer and do not necessarily reflect those of the personnel of the
Survey.

Moore's interpretation of the "Cypress fault" presented on
pages 26 to 29 of the report and shown on figures 5 and 6 does not
conform to that of the Survey staff nor to that of the geologists of





the several oil companies who have worked the well samples of the
area. The section and discussion are presented as the writer gave
them because he believes that they represent an accurate interpre-
tation. Differences in the interpretation of the stratigraphy, par-
ticularly in the details of the division of the Ocala group of Florida
also exist. It is anticipated that Florida Geological Survey Bulletin
38 will be a comprehensive regional evaluation of the stratigraphy,
paleontology and facies of the Ocala group in Florida.

Respectfully yours,

Herman Cunter, Director


































Printed by E. O. Painter Printing Company, DeLand. Florida






FOREWORD


This study of Jackson County was made possible by a coopera-
tive agreement between the Department of Geology, Cornell Uni-
versity, Ithaca, New York, and the Florida Geological Survey,
Tallahassee, Florida. The Department of Geology at Cornell Uni--
versity furnished laboratory facilities; the Florida Geological Sur-
vey provided financial assistance, field equipment, and supervision
of the field work.
The writer was assisted in the field by temporary employees of
the Florida Geological Survey: Mr. T. W. Lins, in the summer of
1947, and Mr. Neil FitzSimmons in the summer of 1948. The late
Mr. Clarence Simpson, Florida Geological Survey, assisted the
writer at intervals during the summer of 1949.
Dr. W. Storrs Cole, Chairman of the Department of Geology,
Cornell University, supervised the research. Dr. C. M. Nevin and
Dr. J. W. Wells of that department gave freely of their time for
discussion and criticism throughout the study. Dr. Herman Gunter,
Director, and Dr. Robert 0. Vernon, Assistant Director, of the
Florida Geological Survey supervised the field work.
The writer wishes to thank the faculty of Cbrnell University and
his colleagues at the Virginia Polytechnic Institute who willingly
gave much time to discussing the problems encountered in this work.
The writer wishes to thank Mr. J. T. Hurst, 1945-49 Supervisor,
and Mr. George Vathis, 1950-54 Supervisor of the State of Florida
Department of Conservation, and Dr. Herman Gunter, Director,
Florida Geological Survey, for their financial aid. Dr. Gunter, Dr.
Vernon, and Dr. J. L. Calver of the Florida Geological Survey ac-
companied the author in the field on several occasions. Dr. Vernon
frequently discussed with the author the problems of stratigraphy
and Pliocene-Pleistocene terrace surfaces in this area.
The author wishes to express his appreciation for the financial
assistance granted him under the Shell Oil Fellowship in Geology
during the academic year 1949-1950.
The late Professor Emeritus G. D. Harris, and Dr. K. V. W.
Palmer of the Paleontological Research Institute examined the
palecypods and gastropods from the Lepidocyclina (Nephrolepi-
dina) chaperi zone. Dr. C. Wythe Cooke, United States Geological
Survey, studied the echinoids collected from the L. (N) chaperi
zone.
The citizens of Jackson County, through their interest and as-
sistance, contributed much to the successful completion of the study.
The water well drillers of Jackson County deserve special thanks





for their assistance in collecting samples from wells. Those who
contributed samples were:

E. J. Carlisle Henry Prestwood
A. C. Clark Gray Artesian Well Co.
B. F. Johnson E. P. Perkins
F. M. Green H. E. Baker

The Coastal Petroleum Finding Company of Houston, Texas,
through Mr. A. D. Aden, supplied many elevations of road corners
and other landmarks, so that the altimeter elevations in this report
are more accurate than would otherwise have been possible.
Mr. Harold Jean Steffan prepared most of the base map for the
geological map, utilizing the Jackson County road map of the Flor-
ida State Road Department as a guide.
Dr. W. D. Lowry, Dr. R. V. Dietrich, and Dr. Mary H. Ross of
Virginia Polytechnic Institute, criticized the manuscript.
The Engineering and Industrial Experiment Station, University
of Florida, Gainesville, Florida, performed the clay tests included
in this report.






CONTENTS


ABSTRACT .. . . . . . . . ..------- ------ .----- iii

LETTER OF TRANSMITTAL .. .............. ...--- --- v

FOREWORD vii

INTRODUCTION ------------- 1
Location --------------- ---- 1
General economy ----------------- 2
Facilities 2-------------------

FIELD METHODS ----------- 3
Location of points -------------- 3
Determination of elevations ------- ------- 4
Maps ------ -------- -- ------------------------------- 4

PREVIOUS GEOLOGICAL WORK IN JACKSON COUNTY -.._-- 4

GEOMORPHOLOGY ------------- 6
General ------------------- 6
Marianna River Valley Lowlands ---------- 7
Delta Plain Highlands -8-. --- ----- ------ 8
Terraced Coastal Lowlands __ --- ----____ __- 9
Development of terraces --------------------------------- 9
Relationship of stream terraces to streams -------- 13
Stream course changes -----------------------. -----....- .- 13
Jointing reflected in stream courses ---- ------- 15
Karst topographic features ----------- 16
Steepheads ...-- ----------------__-- 17

STRATIGRAPHY, PALEONTOLOGY, AND STRUCTURE -----. 18
Introduction -- .-- ..-----...-- ----.. ---- -------_..._.___... -- 18
Eocene Series ... .---------------. -------... . . . . ..-----------.. --- 20
General _--- ----- ---------- 20
Moodys Branch formation and equivalents ----- -- 22
Cypress fault --- .----- -- -- -- __ __- 26
Ocala group -- ------- 29
H history .--- ---------------------.............. -------- 29
Crystal River formation ------------------------... ..--.. .. 30
Historical ------. .--------. -------------------.---------- 30
D definition ..----------- -- -- -------------.... .. ... . .... ....__ __.. 31
Lithology --- _._------.--. -......- ----------------... 31
Thickness and structure ----------- 32
Paleontology ------32
Local details ------------ ----- 32
Bumpnose member of the Crystal River formation --..------ 36
Historical .... - -----------... .. .... 36
Definition -----.... ......------ _. .__....... .._.___ . .._ ....._... ._ 40
Lithology ---.-- ........ ......-- ----- ---. .- ... -... ......... .__... 40
Thickness ------------------... ------ ----- -.._.. ..... 40
Paleontology .---------------- --- ------- -------...... .. .---_ 40
Local details --- ------------... -__ -----.___ -- __--. .... .. . 41






Gadsden limestone ------------- 42
Historical -..------------ ---------------- 4........ . 42
Definition .--.- ----- -- 43
Lithology --... .. .___....... -- 44
Thickness and structure -. --------- --- 44
Paleontology ------------------ -- 44
Local details -..... ---------------------------... --.... _- 44

Oligocene Series ....-------- -- -- - --- 44
Marianna limestone -------------- 44
Historical ...-------------- 44
Definition .----- --------- -----... ..--------.- ----- 44
Lithology .....--- --- ----- -----------.....-----.--... --------- 45
Thickness and structure --------- 45
Paleontology ---------------- 45
Local details -- 45

Vicksburg group and Chickasawhay marl ---- 51
Suwannee limestone -------------51
Historical -.. --------.--_ .. ---- 51
Definition ... ------------- ----- 51
Thickness and structure -- ----------- 51
Paleontology ........---- ---------.. ------- ..- 53
Local details ------------------ 55

Miocene Series ....-------- -----. ----------.-- --..- -.......-- .----- 58
Tampa formation ..... ------------------.-.-..--.----- 58
Historical -- --------- ------------------------ 58
Definition --------- -------- 58
Lithology --------- -- ---- 58
Thickness and structure ...--------- 58
Paleontology --. ----------- -------------- 59
Local details ------------ ------ 59

Post-Miocene deposits _. ------. -----------69
Historical ......--------- ------ 69
General discussion --------- -------- 69
Lithology and thickness ------------ 71
Residual boulders -- 71

SEDIMENTATION, BIOFACIES, AND STRUCTURE .---. 71
Biofacies evidence __..-_.---.-......-.------------------ 73
General --- ... ------------.... ---.....- 77
Crystal River formation -------..------------------ 79
Bumpnose member --.---------------- 80
Marianna limestone --------------80
Suwannee limestone ....... -----------------------------------.- 80
Miocene (Tampa) --------....------------- .--- -------- -.- 81
Post-Miocene .--.---------.-- ----......------- 82
Summary -.. -- --. --... .. ...-----.--. .--------.. ... 82

ECONOMIC GEOLOGY ------.-.....--............. .----.-.. .. --------.. -... 82
General ----- .-.- ..---- .- --.-- -... ..------- ---------------.... 82
C lay -- ... -. . . . ---- ---------------. 82






Exploration for clay ...------------ ----.- 84
Sand and gravel --.---------. -----------------..--- 84
Limestone -...--....-.....-------.---------------...... 84
Ground water ...-- ------- -- ---- 885
Petroleum ---- --.-........------- -- ---..-- 87

SELECTED BIBLIOGRAPHY -- ---..-----... -------....----- -- 90

APPENDIX I .....--- ------..-------... .---- --- ......... -97

APPENDIX II --....- ---...... ---- ........ .. -100



LIST OF ILLUSTRATIONS
Page
Frontispiece. Aturia alabamensis (Morton) --.. ------ ii
Figure
1. Location map showing Jackson County -------- 1
2. Angular stream pattern of Chipola River, probably caused by
jointing .-...---------.----...-..... 15
3. Locality J-141. A steephead just north of Alliance --- 17
4. Geologic formations in Jackson County, Florida ----- 19
5. Structure map of the Claiborne Eocene ------ 27
6. Structure map of the Ocala group ...----------- 28
7. Locality J-5, Marianna Limestone Products, Company. Rock
being quarried is Lepidocyclina (Nephrolepidina) chaperi zone,
the Bumpnose member, and Crystal River formation ------ 37
8. Locality J-12. The uppermost bed is the Lepidocyclina (Nephro-
lepidina) chaperi zone. The lower rock is more typical of the
Crystal River formation _-- ..... ------- 39
9. Structure map of the Marianna limestone ---- ------.. 46
10. Suwannee limestone at locality J-78 is overlain by "bentonitic"
clays and terrace deposits. The dark halo surrounding the
white rock is the "bentonitic" clay. The Marianna limestone at
this locality is not shown in this picture ------------- 47
11. Locality J-14. Marianna limestone at Chipola River bridge
east of Marianna on highway U. S. 90 -------------.---...._.... 48
12. Locality J-13. Marianna limestone overlain by Suwannee lime-
stone ---..-- ..----- ------..--------------- ---- 50
13. One of a series of gentle arches in the Tampa formation just
south of Jackson County in Calhoun County on the Chipola
River. North is to the right in the picture ------------- 52
14. Dip of Suwannee limestone at Sink Creek bridge on the Chipola
River ------------....-------- -- ...... 52
15. Map, top of Oligocene sediments .--..--------.... .---------......... 54
16. Map, probable thickness Tampa formation ----- ---- 60





17. Structure map of Tampa formation --- ------- 61
18. Upper part of Tampa formation as exposed at east end of Jim
Woodruff Dam on Apalachicola River, just north of Chattahoo-
chee. in Decatur County, Georgia ---------- 62
19. Composite section of the Tampa formation at east end of Jim
Woodruff Dam. Elevations at 0 feet, 40 feet, and above 122 feet
are accurate. Elevations shown to the left were determined by
levelling ... --- -----_. ---- ---- --63
20. Locality J-195. Tampa formation clays overlain by "bog iron"
and terrace deposits on highway Fla. 276 east of the Florida
Industrial School for Boys -------. 67
21. Locality J-87. Railroad cut at Round Lake showing Miocene?
clays (Alum Bluff?) overlain by terrace deposits --. --- 70
22. Drainage canal south of Malone cut in terrace deposits. Looking
west from highway Fla. 71 ..-----.-- 72
23. Residual boulders of Suwannee limestone in terrace deposits
forming the sides of the drainage canal south of Malone ----..... 72
24. Camparison of foraminiferal faunas of the Bumpnose limestone
and Gadsden limestone. "Large" Foraminifera omitted .------._- 75
25. Isopach map of the upper Eocene, Oligocene, and lower Miocene
formations --- 78
26. Community House, Marianna, Florida. This building is con-
structed of Marianna limestone .-- _-.- 86
27. The residence of Mr. Cecil Rhyne, Marianna, Florida. This
house is constructed of Marianna limestone blocks faced with
ferruginous sandstone -- ---------------- 86


PLATES
Plate
I Geologic Map ---.--------- --- In pocket
II Terrace Surfaces Map _---------- In pocket
III Structure Section A-A' ----- -----In pocket
IV Structure Section B-B' ----- -.---------- In pocket
V Structure Section C-C' ------------- In pocket


TABLES
Table

1. Some Eocene Foraminiferal zones in Jackson County -21
2. Typical Ocala group foraminiferal faunas ----- 33, 34
3. Suwannee limestone foraminiferal check list 55

Appendix I Formational tops in wells ------------ 97

Appendix II Clay sample test data ...--.--- -.------------.---.-.- 100






GEOLOGY OF JACKSON COUNTY, FLORIDA
by
Wayne E. Moore

INTRODUCTION
Location.-Jackson County is located in northwest Florida and
includes an area of approximately 942 square miles which is
bounded by the State of Alabama on the north, the Chattahoochee
and Apalachicola rivers on the east, Calhoun and Bay counties on
the south, and by Holmes and Washington counties on the west
(Figure 1). The ground surface of the county lies from 100 to 320
feet above sea level except immediately along the rivers where
elevations are lower. The City of Marianna is the county seat.


Figure 1.-Location map showing Jackson County.




FLORIDA GEOLOGICAL SURVEY


The county lies within the Coastal Plain Province, and topo-
graphically may be subdivided into the Delta Plain Highlands, the
River Valley Lowlands, and the Terraced Coastal Lowlands. The
rocks that crop out in the county range from upper Eocene to
Pliocene?-Pleistocene in age. (Plate I). Jackson County is struc-
turally high in a regional sense.

General Economy.-Jackson County is one of the principal agri-
cultural counties in Florida. Field crops, other than vegetables,
fruits, and nuts, are the most important source of farm income with
livestock and livestock products second in importance [Bur. of the
Census, 1951, Jackson Co., (59-032) Series AC50-1]. Listed below
are major agricultural items produced [Bur. of the Census, 1951,
Jackson Co., Fla. (59-032) Series AC50-11:

Item Production
1944-45 1949-50
Value of Farm Products sold $ 4,421,935 $ 5,940,158
Field Crops, other than vegetables, nuts
and fruits $2,953,816 $3,539,051
Livestock and livestock products sold $1,066,822 $1,808,713
Forest products sold $ 45,189 $ 101,544
Cattle and calves, number 26,326 20,493
Whole milk sold, gallons 277,986 778,650
Hogs and pigs, number 54,934 49,013
Chickens, number on hand 119,484 87,229
Corn, bushels harvested for grain 631,869 503,636
Peanuts harvested for picking or
threshing, pounds 32,473,281 26,828,092
Lupine seed harvested, pounds 1,864,200
Irish potatoes harvested, bushels 7,436 5,467
Sweet potatoes harvested, bushels 87,340 46,733
Cotton, bales 2,745 3,603
Tobacco, pounds 105,085 141,488
Sugar cane or sorghum sirup, gal. 124,443
Vegetables harvested, for sale $216,253 $130,005
Pecans harvested, pounds 226,307
Tung nuts harvested, pounds 3,258,418

Facilities.-The 1950 Census of Population Series PC-8 No. 9
and No. 9A gives the following population figures for Jackson
County:
1940 1950
Jackson County 34,428 34,645
Alford 283 375
Campbellton 311 307
Cottondale 719 747
Cypress 212 262
Graceville 1,181 1,638
Malone 442 521
Marianna 5,079 5,845
Sneads 727 1,074




GEOLOGY OF JACKSON COUNTY, FLORIDA


The number of farms with electricity increased from 723 in
1945 to 2,134 in 1950, and during this time the average size of
the farms increased from 97.5 acres in 1945 to 123 acres in 1950.
Transportation facilities in the county are adequate. The Louis-
ville and Nashville Railroad crosses the county in an east-west
direction passing through Cottondale, Marianna, and Sneads. The
Atlanta and St. Andrews Bay Railroad crosses the county from
north to south, passing through Campbellton, Cottondale, Alford,
Round Lake, and Compass Lake. The Marianna and Blountstown
Railroad extends southward from Marianna to Blountstown which
is in Calhoun County to the south.
A number of intercity bus lines serve the area and some 50
buses make stops in Marianna each day. A number of intercity
trucking firms serve the area, and the cities of Atlanta, Birming-
ham, Jacksonville, Mobile, New Orleans, Pensacola, and Savannah,
may be reached by overnight truck haul from Marianna.
The Marianna Airport, which is municipally owned, has 36,000
square feet of hangar space, four 5,000 foot runways, and is
equipped with marker lights for night operation. The field is open
to private planes and charter service is available. Commercial
transportation is provided by the National Airlines which operates
one flight daily each way on the Jacksonville-Pensacola route. A
crop dusting service is maintained at the airport.
Adequate water supplies are available in the county, and mu-
nicipal systems are generally large enough for further expansion.
A modern county-owned general hospital is located in Marianna and
has a 100 bed capacity. A state owned tuberculosis rehabilitation
center with a 200 bed capacity is located near Marianna.

FIELD METHODS

Location of Points.-Since the area included in Jackson County
is large, automobile transportation was used extensively to visit
all portions of the county. This means of transportation was supple-
mented by the use of a boat on the major streams, where necessary.
The map locations of collecting localities were determined either
by plotting automobile odometer distances or by locating the sites
on an aerial photograph mosaic of the county by inspection. All
localities along the Chipola River were determined by very careful
reference to aerial photographs.





FLORIDA GEOLOGICAL SURVEY


Determination of Elevations.-Elevations used in this report
were determined for the most part by means of corrected aneroid
altimeter surveys. The elevations of some wells listed in Appendix
I, however, were determined by instrument leveling done by Mr.
Hal Chittum, the late Clarence Simpson, and Mr. George Benedict
of the Florida Geological Survey. The bench mark control for the
altimeter survey utilized United States Coast and Geodetic Survey
and United States Geological Survey bench marks in areas where
they were available. The Coastal Petroleum Finding Company of
Houston, Texas kindly supplied a large number of elevations along
highways and graded roads which they had determined by stadia
methods.
Frequent altimeter readings through each field day at known
elevations and at field stations permitted the construction of a cor-
rection curve for the readings. The altimeter used in the field was
graduated in ten foot intervals and estimations were made to the
nearest two feet. Elevations determined by altimeter were com-
pared with established elevations a number of times. Discrepancies
of more than ten feet were rare. In critical areas repeated altimeter
determinations of elevations made on different days indicated an
accuracy sufficient to show consistently the gentle dip of the beds.
Maps.-The only map readily available for use in the field was
the Florida State Road Department Highway Map of Jackson
County, which was supplemented by the U. S. Department of Agri-
culture aerial photograph mosaic of the county. The Geological
Map of Florida by C. Wythe Cooke (1945) was valuable in evaluat-
ing the relationship of the county to the entire state and the geo-
logic maps of Holmes and Washington counties (Vernon 1942)
were helpful in determining the relationship of the geology of
Jackson County to these bordering counties. The U. S. Engineer,
Apalachicola River System, Topographic Survey maps were useful
in determining features along and near the rivers.

PREVIOUS GEOLOGICAL WORK IN JACKSON COUNTY

Smith (1881) appears to have been the first to report on the
formations in the county and to describe specific localities of lime-
stone in the vicinity of Marianna, south of Campbellton, at Green-
wood, and at Blue Springs. He prepared a geological map of Florida
which included the Jackson County area. Langdon (1889) described
the rocks exposed at the old Chattahoochee Landing and assigned
the name "Chattahoochee group" to them. Dall and Harris (1892,




GEOLOGY OF JACKSON COUNTY, FLORIDA


p. 107) stated that the limestone exposed along the Chipola River
was not the "Orbitoides" as supposed by Smith.

The first systematic work on the geology of Florida was that
of Matson and Clapp (1909). This preliminary report marked the
beginning of a continuing series of publications by the Florida
Geological Survey which has extended to the present time. Matson
and Clapp (1909) did field work in Jackson County and named the
Marianna limestone from the exposures of the "chimney rock" in
the vicinity of Marianna.

During the next few years work in Jackson County was of
minor nature and consisted of reports on clays, a description of
Ocheesee Lake (Sellards, 1910, p. 67), some data on the artesian
water of the county (Sellards, 1912, pp. 119-122), a report on the
geography and vegetation (Harper, 1914, pp. 193-200), and an
analysis of a brick clay (Sellards, 1915, pp. 17-18).

Cooke (1915, p. 109) described a section on the Chipola River
at Marianna and proved that the Marianna limestone was above
the Ocala limestone. In the same report the upper Eocene age of the
Ocala limestone was established. Cooke (1917) discussed the strati-
graphic range of some larger Foraminifera which he had collected
at Marianna and elsewhere, and in the same paper Cushman (1917)
described some of these larger Foraminifera. In 1920 Cushman
described additional species of these fossils from the Marianna lo-
cality. Sellards (1919, p. 128) showed on a sketch map the struc-
tural high which exists in the Marianna-Chipley area, and this was
expanded in 1922 into a report on the petroleum possibilities in
Florida (Sellards and Gunter, 1922, p. 70; p. 108). Bell (1924,
p. 111; pp. 172-173) discussed some of the clays that 'occur in
Jackson County, and Mossom (1925, pp. 145-151) described the
limestones. In 1926 Mossom (pp. 191-208) reviewed and refined
the structure and stratigraphy of the Marianna-Chipley area.
Cooke (1929) published a new report on the geology of Florida in
which many new outcrops in Jackson County were reported.

Cole and Ponton (1930) described the Foraminifera from the
Marianna limestone, and later Cole (1938) studied the stratigraphy
and micropaleontology of the Granberry well in Jackson County.
MacNeil (1944) did work in Jackson County as part of a study of
the Oligocene stratigraphy of the southeastern United States. He
was the first to question the uppermost Ocala age of the zone charac-
terized by the Foraminifera Lepidocyclina '(Nephrolepidina) cha-




FLORIDA GEOLOGICAL SURVEY


peri Lemoine and R. Douville [L. (N.) fragilis Cushman of Mac-
Neil (1944) and others.]
Periodically from 1915 to the present, Cooke visited Jackson
County in connection with his work on the Cenozoic stratigraphy
of the southeastern United States. Cooke (1945) in the latest edi-
tion of the "Geology of Florida," published by the Florida Geological
Survey, again summarized the geology of Jackson County.

GEOMORPHOLOGY

General.-The entire state of Florida lies within the Coastal
Plain province (Fenneman, 1938). Three predominant topographic
levels make it possible to subdivide Jackson County into three minor
units, the River Valley Lowlands, the Delta Plain Highlands, and
the Terraced Coastal Lowlands (Plate II).
Cooke (1939, p. 4; 1945, p. 8) proposed a terminology for the
geomorphic units in Florida. Vernon (1942, p. 5) proposed two new
terms, the River Valley Province and the Coastal Plains Province,
to replace respectively Cooke's terms, the Marianna Lowlands and
the Western Highlands. Vernon proposed this change with a view
toward making the terms descriptive of the origin of the geo-
morphic units.
Vernon's 1942 terms are undesirable in that they are classed
as provinces, a general term used by Fenneman (1938) in classify-
ing the major geomorphic features of the United States. As any
land forms that may be developed in Florida are minor features
within Fenneman's larger unit, the Coastal Plain Province, it seems
advisable to eliminate the word province from any geomorphic
term which may be applied to units in Florida.
Vernon (1951) proposed a new terminology for geomorphic
units in Florida that eliminates these objections. Consultation with
R. O. Vernon and the staff of the Florida Geological Survey re-
sulted in agreement on these points regarding the origin of geo-
morphic units in Florida:
1. Land forms have resulted in part from the erosion of a plain
of aggradation which was built up during a time of relatively higher
sea level than that which exists today. Remnants of this plain of aggra-
dation are present today in western and central Florida. This plain,
called the Delta Plain Highland by Vernon (1951, p. 16), is underlain
by deposits that have been referred to the Citronelle formation by Cooke
(1945). The development of the constructional plain was terminated in
the Pliocene or early Pleistocene, and since that time sea level has
become progressively lower.




GEOLOGY OF JACKSON COUNTY, FLORIDA


2. Two principal degradational processes have operated since early
Pleistocene to produce the geomorphic units observed today in Florida:
a. Dissection and alluviation by present river systems.
b. Coastal erosion and deposition by the sea.
3. Coastal terraces and stream terraces have developed as a result
of a number of periods of relatively stable sea levels, each stable sea
level occurring at a lower level relative to the land than the preceding
one.
The development of these stream and marine terraces will be
discussed later in this report.
The terminology used here for the geomorphic units is that pro-
posed by Vernon (1951, p. 16). These terms refer to the origin of
the unit, and they provide a means of applying a localizing term
where desired. The Delta Plain Highlands refers to the extensive
remnants of a plain of aggradation which include the highest land
areas in Florida. The Terraced Coastal Lowlands include those
areas where marine terraces are distinctive features of the land
surface. The River Valley Lowlands are the terraced lowlands de-
veloped by erosion and deposition of streams. Vernon's term, the
Tertiary Highlands (1951, p. 16), is not used in Jackson County
because this unit is not represented.

Marianna River Valley Lowlands.-The Marianna River Valley
Lowlands is the largest physiographic unit in Jackson County. This
terraced lowland has resulted from erosion and deposition by a num-
ber of streams, namely the Chattahoochee-Apalachicola rivers, the
Chipola River, Dry Creek, and Holmes Creek. The lowlands along
each of these streams, developed as floodplains and terraces, are
considered as one physiographic unit that was developed in the
Marianna area by a complicated sequence of stream erosion, de-
position, and capture. Elsewhere in the state the lowlands along
streams can be specifically related to the stream now occupying the
valley in which the lowlands are developed. This terraced lowland
extends westward into Holmes and Washington counties where the
Choctawhatchee River and Holmes Creek are responsible for its
development. Although this area is underlain by limestone, solu-
tion is not primarily responsible for the development of the low-
lands. Solution is at present modifying the lowlands, but exposure
of the limestones at the surface, by the removal of overlying plastic
sediments, is so recent that no appreciable lowering of the surface
can be attributed to solution. It is a lowland produced by the dis-
section of the Miocene formations. This erosion was accelerated by
the lowering of sea level during the maxima of continental glacia-
tion.





FLORIDA GEOLOGICAL SURVEY


Most of the sediments deposited in Jackson County from Tampa
time until early Pleistocene time, when active downcutting began,
were increasingly plastic in nature. When a reasonable restoration
of these sediments is made from the dip of the Miocene and post-
Miocene beds in Jackson County, it is apparent that a considerable
thickness of plastic sediments has been removed from the area
occupied by the Marianna River Valley Lowlands.
As a result of this erosion the normal cuestaform topography of
a coastal plain rather than karst topography has been formed.
The configuration of the Marianna River Valley Lowlands is con-
trolled by the location of major surface streams (Plate II).
The Flint River and the Apalachicola River occupy approxi-
mately the position of a subsequent stream when the structure of
the area is considered. The prominent escarpment at Chattahoochee,
which extends northeastward into Georgia along the south side of
the Flint River system is the infacing escarpment that marks the
east boundary of the Marianna River Valley Lowlands.
Erosion by Dry Creek, a subsequent stream in the southwestern
part of Jackson County, has produced a north-facing escarpment
that limits the Marianna River Valley Lowlands to the south.
In the southeastern part of Jackson County the small streams
which are tributary to the Chipola River and which extend east
and northeast from Sink Creek have produced a north-facing es-
carpment which forms the other boundary of the Marianna River
Valley Lowlands. The Marianna River Valley Lowlands extend
westward from Jackson County into northern Washington County
and into Holmes County, but there the lowlands can be specifically
identified with the Choctawhatchee River and Holmes Creek, and
may be called properly the Choctawhatchee River Valley lowlands
(Vernon, 1951, p. 16). With the exception of the westernmost part
of the county where the lowland is related to Holmes Creek, the
lowland in Jackson County is associated with streams of the Apa-
lachicola River system.
Delta Plain Highlands.-The Delta Plain Highlands include
that part of Jackson County south of Dry Creek and north of
Compass Lake extending eastward to about the center of R. 10 W.
This area is characterized by elevations generally above 240 feet.
Elevations as high as 320 feet were measured in sections 25 and 26,
T. 3 N., R. 12 W. between Compass Lake and Round Lake. Cooke's
topographic division, the Western Highlands, and possibly the Cen-
tral Highlands, are remnants of this surface.





GEOLOGY OF JACKSON COUNTY, FLORIDA


Terraced Coastal Lowlands.-The Terraced Coastal Lowlands
in Jackson County lie south of the Delta Plain Highland, and in the
southwestern part of the county extend southward from Compass
Lake. An extensive high flat area that is present east of the Chipola
River southward and eastward from Alliance probably belongs in
the Terraced Coastal Lowlands, but it may have been developed
by streams.
Development of Terraces.-Three stream terraces, one marine
terrace, and an older dissected highland are found in Jackson
County in addition to the present flood plains (Plate II). As prev-
iously pointed out by Vernon (1942, 1951), each marine terrace
has fluviatile equivalents in each major stream valley in Florida.
In Jackson County these stream terraces lie at intervals above the
present flood plain of 30-50 feet (Pamlico), 60-100 feet (Wicomico),
and 145-165 feet (Okefenokee). Vernon (1951, p. 40) uses the
names assigned to the marine terraces by Cooke (1945) as modi-
fied by MacNeil (1950) to apply to the stream terraces as well.
This simplifies the terminology required to discuss these terraces,
and Vernon's practice will be followed here.
The stream terraces in Jackson County have slopes approxi-
mately the same as those of the flood plains of the present streams
which occupy the valleys where the terraces are found. The highest
fluviatile terrace, the Okefenokee, may not have a slope parallel to
the present flood plains, as its slope has not been determined ac-
curately.
The marine terrace, the Coharie, has a maximum elevation in
Jackson County of 240 feet north of Compass Lake, and it slopes
seaward to a minimum elevation of about 170 feet south of Jackson
County (Vernon, 1942, p. 17). Above the marine terrace is an older
dissected highland which has a maximum elevation of 320 feet
and which generally lies above 270 feet.
Similar terraces have been observed in coastal plain areas in
many parts of the world. The widespread occurrence of these ter-
races, separated everywhere by approximately the same intervals,
has caused them to be cited as examples of evidence of changes in
sea level. In recent years the origin of these terraces has been at-
tributed by Antevs (1928, 1929), Daly (1925, 1929), Fisk (1938,
1939, 1940), Russell (1940), Vernon (1942, 1942a, 1947, 1951),
Cooke (1945), and others, to sea level fluctuations during the Pleis-
tocene when large quantities of water were removed from the sea
and locked temporarily in the continental glaciers. In this theory




FLORIDA GEOLOGICAL SURVEY


it is proposed that, while sea level was falling and rising as the
glaciers advanced and retreated, the land gradually stood higher
relative to the present sea level in the areas where these terraces
are preserved. In this way when sea level reached a new maximum
height during glacial minima, it would not reach its former level
on the land and the terraces formed during the previous maxima of
sea level would be preserved. Attempts have been made to cor-
relate these terraces with the various glacial advances.
In Jackson County the three major stream terrace levels are
related in general to the present streams of the area. Between each
of these major levels there are minor terraces, especially between
the two highest terraces.
Above the stream terraces there is present, in the extreme
southern part of the county, a marine terrace, the Coharie, with a
maximum elevation of about 240 feet. This terrace can be traced
in Jackson County (with the exception of the Chipola River Valley)
from the vicinity of Compass Lake eastward to the Sneads area
where remnants of it are preserved as summits of high, flat-topped
hills. The high, flat plain around and immediately south of Alliance,
in the south central part of Jackson County, represents the best
development of the Coharie terrace. The Coharie terrace extends
from Jackson County eastward into Gadsden County and west-
ward into Washington County.
The stream terraces are progressively younger from highest
to the lowest. This is confirmed when the degree of dissection of
the terraces is considered, for the higher surfaces are most dis-
sected and the lower surfaces are least dissected. The higher sur-
faces are frequently represented only by the flattened summits of
isolated hills, and the deposits show evidence of greater weathering,
especially oxidation of iron, as compared to lower surfaces. Lower
surfaces also tend to retain more of the flood plain features than
do the higher terraces.
This arrangement of the terraces, with the oldest at high ele-
vations and the youngest at low elevations, suggests one of three
possibilities: 1, the land has risen intermittently relative to sea
level; 2, the sea level has fallen eustatically in stages; or 3, the land
has risen uniformly as sea level dropped and rose eustatically to
its former level several times. Locally, it is frequently impossible to
separate the effects of the first two possibilities for the end results
may be the same. Sea level changes, however, produce world wide
effects which indicate changes of the same amount taking place in




GEOLOGY OF JACKSON COUNTY, FLORIDA


the same direction at the same time. Vertical movements of the
land are apt to be local, to occur at different times, and to be in
different directions in various places. The third possibility has
been used by Fisk (1938) to explain stream terraces in Louisiana.
According to the theory of stream terrace development outlined by
Fisk (1938, p. 67-72; 1940, p. 57) and extended to Florida by Ver-
non (1942, p. 26), each of the terrace levels represents a period of
valley cutting followed by drowning and alluvial filling of the river
valley. The periods of valley cutting occurred during glacial per-
iods when sea level was lowered, and the period of drowning and
alluvial filling coincided with the warm interglacial periods when
the glaciers retreated.

A period of valley cutting followed by a period of valley alluvia-
tion compose a cycle, and the surface of the alluvial fill would cor-
respond in elevation with the previous flood plain unless uplift of
the landmass occurred during the cycle or unless sea level was pro-
gressively eustatically lowered, in which case the new alluvial fill
would be below the previous flood plain by the amount of relative
uplift which occurred during the cycle.

In Louisiana, Fisk (1938, p. 69; 1939, p. 199) and Russell (1940,
p. 1225) demonstrated tilting based upon the steeper slopes of the
older terraces as compared to the younger terraces. This theory
seems to apply most logically to the origin of stream and delta plain
terraces in Louisiana.
In Jackson County, however, no tilt between the Pamlico and
Wicomico stream terraces could be detected though hundreds of
controlled altimeter elevations were taken. These lower terraces
have a slope that is essentially that of the present flood plain of
the Apalachicola River, the Chipola River, and Holmes Creek. The
slope of the Okefenokee surface is not clearly evident as that surface
is well dissected.
The number of terraces observed in the field do not necessarily
mean that there were a corresponding number of major inter-
glacial periods. It is generally agreed, for example, that the climate
has not become as warm since the last major glaciation as was
normal during previous interglacial times or during the period im-
mediately pre-Pleistocene. Sea level will rise if the ice that is at
present located on the continents melts.
Sellards (1916, p. 109; 1918, pp. 86-87) and Vernon (1942, pp. 7,
19-21; 1942a, pp. 302-311; 1947, pp. 97-99) have given evidence




FLORIDA GEOLOGICAL SURVEY


in Florida that sea level is rising, or has very recently risen, based
upon drowned streams both along the coast and inland where tribu-
taries to major streams have been unable to fill their valleys with
alluvium as fast as the major stream.

Estimates for the further rise in sea level that may be expected,
if the climate continues to moderate and all continental ice caps
melt, range from 66 to 165 feet (Flint, 1947, p. 431). If sea level
should rise slowly to 50 feet above its present level, alluviation
would cover the Pamlico terrace, provided the streams could re-
establish or maintain approximately their present gradiants. Simi-
larly, a sea level rise of 100 feet would alluviate the Wicomico ter-
race. Where attempts to correlate marine or stream terraces with
interglacial periods are made, the expected further rise of sea level
and the probable sea level stands during any interglacial periods
proposed should be considered.

Daly's estimate that sea level was lowered some 250 feet below
present sea level at the height of glaciation seems to be of the right
order of magnitude. Shepard (1948, pp. 244-245), however, has
proposed that sea level may have been lowered more than this,
based upon a more extensive glaciation than is generally accepted
and upon an accumulation of glacial ice to greater thicknesses than
generally proposed. Dr. von Engeln (1950, pp. 161-163) proposed
that subcrustal density changes may have operated to raise the land
masses uniformly. It appears certain, therefore, that a sea level
change did occur; that the lowering of sea level amounted to at least
250 feet during the times of maximum glaciation.

Cooke (1945, pp. 245-248) has suggested that a progressive
lowering of sea level permitted the terraces to be preserved, and
that this resulted from periodic increases in the capacity of the
ocean basins caused by lowering of a large segment of the ocean
floor. Such an eustatic lowering of sea level would have world wide
effects, and the theory does not require any uplift of the land to
preserve the terraces formed during maximum sea level stands
during glacial minima.

Uplift has occurred in Florida, or sea level has been eustatically
lowered, since the deposition of the Delta Plain Highlands. This
uplift probably occurred in late Pliocene or early Pleistocene time.
Fisk's general theory of terrace development, sea level fluctuations
coupled with uplift of the land or eustatic lowering of sea level,
seems to explain best the development of these terraces.




GEOLOGY OF JACKSON COUNTY, FLORIDA


Relationship of Stream Terraces to Streams.-The relationship
of the lower stream terraces, the Pamlico and Wicomico surfaces,
to the present streams within the county is rather clear (Plate II).
These terraces generally parallel the existing major streams in
the county, Holmes Creek, the Chipola River, and the Chattahoochee-
Apalachicola River. The deposits underlying these surfaces are
generally from 30 to 50 feet thick, and they are underlain by Ter-
tiary sediments. Locally, Tertiary sediments may come to the
surface of the terraces as silicified pinnacles, and in some areas the
terrace flats and the surface of the Tertiary deposits apparently
are at the same elevation.

The relationship of the Okefenokee surface to existing streams
is not so obvious. In the western part of Jackson County, for ex-
ample, this surface appears to be level in a north-south direction,
but it is generally so dissected that its slope cannot be determined
with certainty.

Stream Course Changes.-The interconnection between the Ma-
rianna River Valley Lowlands and the Choctawhatchee River Valley
Lowlands to the west, and the apparently anomalous slope of the
Okefenokee terrace suggest that a stream pattern different from
that in existence today may have been present in the past. The
existence of what appear to be unusually deep valley fills supports
the idea that major stream courses have been altered, probably by
capture, during the Pleistocene.

Near the road corner in the NW1/4 sec. 22, T. 6 N., R. 10 W.,
there is a buried channel, or one of many large sinks associated
with an old subterranean stream, that is closely associated with a
high hill which seems to be a remnant of a surface possibly as
high as the Wicomico surface. According to various water well
drillers and the reports of residents concerning the depth of their
wells to bedrock, this buried channel extends north-northeast into
Alabama, a general direction that will join the valley of the Chat-
tahoochee River in the vicinity of Gordon, Alabama. A well drilled
at the road corner mentioned above, indicates that the floor of the
channel was buried to a depth of more than 220 feet below the
present surface, which has an elevation of approximately 130 feet.
A linear topographically low area, not connected with present sur-
face drainage, exists west-northwest of Malone in the center of
the N1/2 sec. 34, T. 7 N., R. 10 W. and it can be seen on the aerial
photograph mosaic, part 3, photograph 11A-39. This topographic





FLORIDA GEOLOGICAL SURVEY


low may be caused by compaction of the sediments filling the buried
channel.
West of the Chipola River, near the top of an abrupt hill which
crosses Highway Fla. 75 in the N.W.1/4 sec. 5, T. 5 N., R. 11 W., wells
were reported which were drilled to depths of nearly 200 feet with-
out encountering bedrock.
The relationships of the stream terraces and the presence of
an assumed stream channel suggest that at some time in the past
a sizeable stream existed where today no stream flows. This sup-
posed stream may have initiated the dissection of the Marianna
River Valley Lowlands. Its buried channel, as inferred from records
obtained from water well drillers, extends northward toward the
present Chattahoochee River. Therefore, it is possible that the
Chattahoochee River once occupied the channel and flowed south-
west across Jackson County.
As pointed out previously, the Apalachicola River and the Flint
River are subsequent streams developed at the base of the north-
west-facing Miocene escarpment at Chattahoochee in Gadsden
County. In this area the presence of the lower stream terraces on
the west side of the river and their absence on the east side of the
river indicate that the Apalachicola River and the Flint River
have been shifting their channels laterally in a southeasterly direc-
tion within relatively recent geologic time.

A submarine valley, the DeSoto Canyon, lies off the Appalachi-
cola delta in the Gulf of Mexico (Shepard, 1948, pp. 213-214, also
fig. 65, p. 179). The depth of this canyon is of the same order of
magnitude as the depth of the buried channel in Jackson County,
if it is assumed that the Jackson County channel was cut from the
surface of the Delta Plain Highland, which has an elevation of 320
feet where it is preserved in the southern part of the county. It
cannot be proved that the buried channel and the submarine valley
are related, because sufficient data are not available at present.
Nevertheless, the magnitude of these valleys suggests the possi-
bility of interconnection.

Shepard (1948, p. 215) notes that the closed depressions in the
bottom of the DeSoto canyon are not typical of most submarine
canyons. A projection of the probable structure of the Oligocene
and Miocene limestone beds, based upon data from the Jackson
County area and the Port St. Joe test well studied by Cole (1938,
pp. 8-16) indicates that Miocene limestone may be present at the




GEOLOGY OF JACKSON COUNTY, FLORIDA


submarine ground surface and that these depressions may be solu-
tion holes developed in Miocene limestone.
Jointing Reflected in Stream Courses.-In certain areas of
Jackson County the stream courses exhibit a rectangular pattern
which can be observed on the aerial photograph mosaic. This pat-
tern suggests a control by fracturing, and may be observed along
the Chipola River and Dry Creek in the area where they join (Fig.
2). In that area both streams are flowing on bedrock of Suwannee
limestone. Southward from this area the regional dip increases and
structural evidence in Jackson County indicates a post-Suwannee-
pre-Tampa flexure or fault may have produced the jointing. In
Calhoun County to the south there is evidence that this structural
movement continued into early Miocene time as indicated by several
small folds in the Tampa formation. The Jackson County portion
of this structure, which is interpreted as a fault, is shown on Struc-
ture Section A-A' (Plate III).


Figure 2.-Angular stream pattern of Chipola River, probably caused
by jointing.





FLORIDA GEOLOGICAL SURVEY


The rectangular stream patterns around the junction of the
Chipola River and Dry Creek are believed to be developed along
tensional fractures and the small folds in northern Calhoun County
are compressional folds developed during the early Miocene. A
mantle of soil and terrace sediments prevented direct observation
of these joints, but structural-stratigraphic evidence and the stream
patterns indicate that the fractures are present.
West of Cottondale a number of creeks exhibit a rectangular
stream pattern, as shown on part 5, photograph TU-13A-63, De-
partment of Agriculture aerial photographic mosaic, and the geo-
logic map, Plate I, in sec. 29, T. 5 N., R. 12 W. Unlike the Chipola
River-Dry Creek area, these creeks flow on alluvium, which is from
30-100 feet thick. Examination of the area failed to reveal any ap-
parent reason for the generally rectangular pattern, but since the
patterns are comparable to those on the Chipola River, it is probable
that fractures in the bedrock extend through the mantle. In south-
ern Jackson County, joints, often clay filled, have been developed
in the sediments of the higher terraces. The average strike of these
joints in southwestern Jackson County and southeastern Washing-
ton County agrees generally with the trends of the rectangular pat-
terns formed by the creeks west of Cottondale. The course of these
creeks may be controlled to a considerable extent by jointing which
has developed in terrace deposits. The joints in the terrace sedi-
ments may have been formed by adjustments of the terrace sedi-
ments to fractures in the underlying Tertiary bedrock.
Karst Topographic Features.-Sinkholes and caves, resulting
from solution of limestone, are developed widely in Jackson County,
and are forming today. Their distribution and their relationship to
the terrace topography indicates that ground water saturation of
the limestone, now and in the past, has controlled their formation
to a considerable extent. Most of the caves are located in the out-
crop area of the Marianna limestone, which frequently forms the
roof rock of the cave. Many caves are formed in the Bumpnose
limestone member of the Crystal River limestone.
Although solution is actively lowering the land surface in
Jackson County, the Marianna River Valley Lowlands do not owe
their elevations to solution processes. As already noted, structural
stratigraphic, and terrace surface relationships indicate that these
lowlands resulted from the development of normal cuestaform
topography by stream erosion. Only during the relatively recent
geologic past has solution assumed a dominant role in lowering the
land surface.





GEOLOGY OF JACKSON COUNTY, FLORIDA


Steepheads.-As indicated by Sellards (1918, p. 27) and Ver-
non (1942, p. 29), these features develop as the result of a combi-
nation of these factors:
1. The development of an escarpment that is:
a. Capped by thick deposits of unconsolidated, permeable sand,
and,
b. Underlain by thick, soft, impermeable clays.
2. Abundant rainfall in the area.
3. Obsequent streams which extend up the face of the escarpment.
The steepheads develop from sapping by springs, which emerge
at the contact of the overlying permeable sand and the underlying
impermeable clay. The water which falls as rain seeps downward
through the permeable sand until it reaches the impermeable clay.
As downward movement is checked by the clay, the water begins to
move laterally, emerging at the surface as springs or seeps which
flow down the face of the escarpment in an obsequent direction. At
the site of a spring the moving water tends to remove some of the
sand and clay, thus undermining the overlying sand which slumps
downward leaving a steep headward termination of the stream.
A steephead developed in the above manner near Alliance in Jack-
son County is illustrated in figure 3. This steephead is actively
eroding headward, and recently has cut across the road.








4


Figure 3.-Locality J-141. A steephead just north of Alliance.





FLORIDA GEOLOGICAL SURVEY


STRATIGRAPHY, PALEONTOLOGY, AND STRUCTURE

Introduction.-The bedrock that crops out in Jackson County
ranges in age from upper Eocene to lower Miocene (Plate I). It is
possible that in the southwestern part of the county deposits of
middle Miocene age are present, but no fossils were found to in-
dicate an age for these deposits, which are not noticeably different
lithologically from deposits of lower Miocene age. The oldest forma-
tion that crops out is the Crystal River formation of Upper Eocene
age, and the youngest is the Tampa formation, of lower Miocene
age. The gravel, sand, and clay deposits underlying the terrace
surfaces represent deposition during the interval between the
Miocene and the Recent. As no fossils were found in these beds,
they are considered to represent the Pliocene-Pleistocene interval.
Figure 4 shows the formations found in Jackson County.

Cole (1938, pp. 19-36) reported in detail the stratigraphy and
paleontology of the older formations underlying the county, based
on the samples from the oil test well, Granberry No. 1. The various
formations penetrated in this well are:

Tertiary formations Depths in feet
Ocala limestone 0-220
Claiborne group 220-723
Wilcox group 723-1726
Salt Mountain limestone 1406-1600
Nanafalia formation 1600-1726
Midway group 1726-1937

Upper Cretaceous formations
Selma formation 1937-2879
Eutaw formation 2879-3454
Tuscaloosa formation 3454-5022

The water well drillers of Jackson County collected many well
samples for the Florida Geological Survey during the course of this
study to aid the interpretation of the subsurface stratigraphy and
structure, but no attempt has been made in this study to determine
the stratigraphy and structure below the Lepidocyclina (Poly-
lepidina) antillea zone of Claiborne age. Most of the water well
samples used in this study were cable tool samples. These wells
will be referred to by the Florida Geological Survey well file num-
ber, and all samples are on file at the Florida Geological Survey.
Appendix I contains logs of the wells referred to in this report.





GEOLOGY OF JACKSON COUNTY, FLORIDA


Figure 4


Geologic Formations in Jackson County, Florida


ER PERIOD EPOCH FORMATION


RECENT


PLEISTOCENE


>-



z



I--
4





a


















4
I-




>-




l--



I--


River floodplain alluvium


Marine and fluvial terrace deposits
Pamlico formation

Wicomico formation

Okefenokee formation

Cohorie formation




Possibly sediments of the
Delta Plain Highlands


Tampa formation. Beds of Alum
Bluff age may be present in
southwest Jackson County


OLIGOCENE Suwannee limestone
Marianna limestone


-~ 4


UPPER


Bumpnose Is.mbr.
S- Gadsden Is.
(subsurface
Ocala Crystal only)
Group River
formation


MIDDLE Beds of Cook Mountain age
MIDDLE(subsurface only)
(subsurface only)


PLIOCENE



MIOCENE


L 'J




FLORIDA GEOLOGICAL SURVEY


EOCENE SERIES'
General.-A number of deep wells were completed late in the
preparation of this report which permitted a study of the relation-
ships between the middle and upper Eocene formations in Jackson
County.

Vernon's report on the geology of Citrus and Levy counties
(1952) raised the question of the possible existence of beds of
Moodys Branch age in Jackson County. Further, Puri (1953)
proposed a new classification for the rocks of Jackson age in
Florida by defining the formations within the Ocala group and by
naming formations to subdivide the "Ocala limestone."

No attempt was made to study the middle Eocene for this re-
port, other than to determine the faunal zones that appear in its
upper part so that the nature of the Jackson-Claiborne boundary
in Jackson County could be determined.
Seven Eocene zones are recognized in Jackson County,
and they are shown on the structure sections (Plates III, IV, V).
These zones are based upon the first appearance of the species in
well samples (Table 1).
The Eocene zones in Table 1 require little discussion except
to point out that the Camerina guayabalensis-Lepidocyclina (Plio-
lepidina) ariana zone has been mistaken frequently for the Moodys
Branch formation and in other cases Lepidocyclina (Pliolepidina)
ariana has been misidentified as Lepidocyclina (Polylepidina) an-
tillea (=L. (P.) gardnerae). The zones listed above are Claiborne
in age rather than Jackson because of the presence of Operculi-
noides sabinensis, a species not found in the Jackson stage. Gravell
and Hanna (1940, pp. 412-416) proposed the names Camerina
barker, Camerina mississippiensis, and Lepidocyclina (Lepido-
cyclina) clairbornensis for the species characterizing this zone.
Cole (1944, p. 26) pointed out that Lepidocyclina (L.) claibornensis
was a synonym of L. (Pliolepidina) ariana, and that (Cole 1944,
pp. 39-40) Camerina mississippiensis was a synonym of Camerina
guayabalensis. Cole's practice is followed here. In Jackson County,
Camerina guayabalensis and Camerina barkeri appear to occur to-
gether. Camerina barkeri is dominant in the upper part and Cam-
erina guayabalensis is dominant in the lower part of the middle
Eocene zone.


'Please refer to the Letter of Transmittal.






TABLE 1
SOME EOCENE FORAMINIFERAL ZONES IN JACKSON COUNTY__

SNorthwestern Jackson County Southeastern Jackson County
a 0
rn West of the Cypress Fault East of the Cypress Fault


Crystal Bumpnose member, Lepidocyclina (Nephrolepidina) Gadsden limestone 0
chaperi zone, 0-15 feet. Uvigerina zone, o
b River
o lower member, 0-180 feet.
0
9 formation Operculinoides ocalanus-Asterocyclina
' U zone, 140-160 feet.
40
Operculinoides jacksonensis zone, 30-40 feet

-_-------------- Unconformity ------------------------

a Lisbon Operculinoides sabinensis zone, 10-20 feet

Formation Camerina guayabalensis-L. (Pliolepidina) ariana
b W zone, 50-60 feet

-V L. (Polylepidina) antillea zone, total thickness not determined but at
E E least 40-60 feet.

o Middle Eocene not studied stratigraphically lower.
o


__ ___________________________________________i-




FLORIDA GEOLOGICAL SURVEY


Cole (1944, p. 34) listed the species Lepidocyclina (Pliolepidina)
ariana, Camerina guayabalensis, and Operculinoides jennyi as oc-
curring above the Lepidocyclina (Polylepidina) antillea zone in well
W-336, Nassau County, Florida. Cole (1944, pp. 45-47) expressed
the opinion that 0. jennyi might be a synonym of 0. sabinensis.
These two Operculinoides species are closely related, appear to oc-
cur at the same horizon, and are probably synonyms as suggested
by Cole. Specimens of this type are herein referred to the species
0. sabinensis. In Well W-336, Cole found 205 feet of beds be-
tween the base of the Jackson Eocene and the top of the Lepidocy-
clina (Pliolepidina) ariana zone. These beds, characterized by
Coskinolina floridana, Dictyoconus americanus, and other species,
were not found in Jackson County. The absence of these beds in
Jackson County indicates an unconformity at the top of the Clai-
borne in Jackson County.

The Operculinoides sabinensis zone is distinctive and is the most
useful marker for the top of the middle Eocene in Jackson County.

MOODYS BRANCH FORMATION AND EQUIVALENTS
The presence or absence of beds of Moodys Branch age in Jack-
son County has been a subject of debate. Certain of the Jackson
County well logs on file at the Florida Geological Survey have re-
ferred portions of the Eocene to the Moodys Branch. The beds in
Jackson County generally referred to the Moodys Branch have been
the calcareous, glauconitic sands that underlie the limestones of
the "Ocala limestone." These beds definitely are not of Jackson age
and must be assigned to the middle Eocene. These sandy glauconitic
beds carry Lepidocyclina (Pliolepidina) ariana, Camerina guaya-
balensis, Operculinoides jennyi, and Camerina barkeri, all of which
are middle Eocene fossils and which elsewhere in Florida lie below
the Coskinolina floridana-Dictyoconus americanus zone of accepted
middle Eocene age. It is true that these sandy, glauconitic beds are
lithologically similar to beds of accepted Moodys Branchlage farther
to the west in Alabama. Faunally the beds are not to be correlated,
although the faunal elements are generically similar because of
the similar environments of deposition which are indicated by com-
parable lithologies.

Beds of Moodys Branch age, if present in Jackson County, must
be found in the limestones that have long been referred to the "Ocala
limestone" and which are here referred to the Ocala group (Puri,
1953, p. 34). Puri lists the following faunal zones for the Williston




GEOLOGY OF JACKSON COUNTY, FLORIDA


formation and the Inglis formation in Florida (Moodys Branch
equivalents in peninsular Florida) :

Williston formation
Nummulites moodybranchensis faunizone
Operculina mariannensis-Nummulites jacksonensis faunizone
Inglis formation
Periarchus lyelli floridanus faunizone

In Jackson County no specimens were found that could be referred
to Operculinoides moodysbranchensis (=Nummulites moodys-
branchensis; see Cole 1952, p. 10 for synonymy). Operculina mari-
annensis occurs near the top of the Crystal River formation in
Jackson County, below the Bumpnose limestone member, and has
been identified at a number of lower horizons in the Crystal River.
It remains one of the better markers for the top of the Crystal
River formation in Jackson County. The uppermost beds of the
lower member of the Crystal River ("Ocala limestone") at the
river bridge just east of Marianna, Jackson County, is the locality
from which 0. mariannensis was originally described. Operculi-
noides jacksonensis (=Nummulites jacksonensis, see Cole 1952,
p. 9 for synonmy) does occur in Jackson County in the lower part
of the Ocala group. If Moodys Branch equivalents exist in Jackson
County, they must be represented by the beds containing 0. jack-
sonensis. The O. jacksonensis zone may not be equivalent to the
Moodys Branch formation, however, because:

1. The species of the Moodys Branch formation are not confined
to the 0. jacksonensis zone in Jackson County and some of the
species range as high as the Bumpnose limestone member of the
Crystal River limestone.
2. There is no lithologic reason to separate the zone from the
Crystal River limestone.
3. Faunal indications that the Jackson County area was struc-
turally high during Jackson Eocene and the existence of an un-
conformity at the top of the middle Eocene, suggest that the Jackson
County area may not have been covered by the sea during Moodys
Branch time.

Vernon (1952, pp. 158-159) lists the following Foraminifera
as the most abundant and prominent of the "Ocala (Restricted)"
fauna: Lepidocyclina ocalana, Camerina jacksonensis, C. vander-
stoki, C. moodysbranchensis, Operculinoides vaughani, 0. willcoxii,
and Heterostegina ocalana. Of these species, Puri (1953, p. 34)





FLORIDA GEOLOGICAL SURVEY


cites C. moodybranchensis and C. jacksonensis as zone markers
for the Moodys Branch equivalents. Vernon (1952, p. 111) corre-
lated the Inglis formation with the Applins' (1944, p. 1683) lower
member of the Ocala limestone. The Applins (1944, p. 1684) state,
"In west Florida where the Ocala is chiefly cream-colored chalk, it
is not possible at present to recognize the two members seen in
the peninsular area." Vernon's check list of Foraminifera in the
Moodys Branch formation (1952, table 10) lists Amphistegina pin-
arensis cosdeni as occurring in the Inglis and the Williston forma-
tions, Moodys Branch equivalents. Applin and Applin (1944, p.
1685) state, in referring to the fauna of the lower and upper
member of the Ocala,

Amphistegina pinnarensis Cushman and Bermudez var. lawsoni n.
var. ... is common in the lower member and may be called its key fossil
on the peninsular, but where present in north and west Florida and
Georgia, it apparently mingles with typical species of the upper member
and has there no zonal significance.
Further, Applin and Jordan (1945, p. 130) state,

The lower member of the Ocala is clearly defined in nearly all well
sections studied from the peninsular area of Florida, but could not be
distinguished from the upper member in northern Florida and southern
Georgia, where lower and upper species seem to mingle in a relatively
thin Ocala section.
Gravell and Hanna (1935, p. 330) list the following species as
occurring in the Moodys Branch:
Camerina jacksonensis
C. moodysbranchensis
Operculina vaughani
Lepidocyclina (Lepidocyclina) mortoni (=-L. (L) montgomeriensis)
Discocyclina flintensis
Discocyclina 2 spp.
As indicated above, Camerina jacksonensis and C. moodysbranch-
ensis are not restricted to the Williston formation or to the "lower
Ocala." Lepidocyclina (Lepidocyclina) montgomeriensis occurs
throughout the Ocala group in Jackson County. Cole (1952, p. 4,
locality 140) lists Pseudophragmina (Proporocyclina) flintensis
(-Discocyclina flintensis) and Operculinoides vaughani (=Oper-
culina vaughani) as occurring in the L. (N.) chaperi zone in the
Panama Canal Zone, so that these species can be considered only as
Jackson Eocene markers. Therefore, in Jackson County those
species that have been cited as being characteristic of the Moodys
Branch formation do not have zonal significance for determining
whether beds there should or should not be correlated with the
Moodys Branch. These species do indicate a Jackson age, however.




GEOLOGY OF JACKSON COUNTY, FLORIDA


Faunally, it does not seem wise to attempt to correlate any part
of the Ocala group in Jackson county with the Moodys Branch
formation, with the Inglis formation, or with the Williston forma-
tion. Lithologically, the Ocala group in Jackson County is not
similar to the typical Moodys Branch formation, since it consists
of white to cream colored limestone. No lithologic differences were
noted that would justify the adoption of existing names for Moodys
Branch equivalents or the proposal of new names for such units in
the Jackson County area. The Moodys Branch is believed to be
absent in Jackson County. If it is represented, the Operculinoides
jacksonensis zone is its probable equivalent. The 0. jacksonensis
zone in Jackson County is correlated in this report with the lower
part of the Crystal River formation of Puri (1953). Lithologically
there appears to be no basis for establishing a new stratigraphic
term in Jackson County for the 0. jacksonensis zone, and the beds
should be included in the Crystal River limestone in Jackson County.
The probable absence of Moodys Branch rocks in Jackson County
is not surprising when the stratigraphic sequence is carefully
studied. Beds equivalent to the late middle Eocene Tallahassee
limestone and Avon Park limestone of peninsular Florida are absent
in Jackson County. Wells in Jackson County pass from beds of
upper Eocene age into beds of early middle Eocene (Cook Moun-
tain) age bearing Operculinoides sabinensis, Camerina guayabalen-
sis, and Lepidocyclina (Polylepidina) antillea. The seas evidently
withdrew from the Jackson County area sometime after early
middle Eocene time and prior to late Eocene time. Beds of late
middle Eocene age and Moodys Branch age are therefore absent by
nondeposition or by erosion. The sandy, glauconitic Moodys Branch
formation represents a transgressive lithofacies, and it is my opin-
ion that the Jackson County area was not covered by the sea until
after Moodys Branch time, and that the Operculinoides jacksonensis
zone of the Ocala group represents the initial phase of Crystal
River deposition in Jackson County.
Evidence for a structurally positive position of Jackson County
during late Eocene time, a necessary condition if it is to be the
last area covered by the transgressive Jackson sea, is presented
in more detail later in this report (see p. 71). In Jackson County
the restriction of the Bumpnose limestone (uppermost Jackson
Eocene age) to structurally positive areas, and the occurrence of
equivalent shallow water and deep water biofacies of Crystal River
age indicate that the Jackson County area was structurally positive
during late Eocene time.




FLORIDA GEOLOGICAL SURVEY


CYPRESS FAULT2

A fault that had not been recognized previously was discovered
when the well samples from Jackson County were studied. This
fault is named the Cypress fault because it passes near the town
of Cypress in Jackson County.
The Eocene faunal zones used in this report maintain a rela-
tively constant thickness in Jackson County. A marked disconti-
nuity was observed in three wells, however. Some 40 to 50 feet of
the Ocala group is missing in wells W-1356 and W-1358. The top
of the Ocala group appears at a lower elevation than expected in
well W-1364, and, though a 100 foot interval of sample is missing
at the Ocala-Claiborne group contact, the interval between the top
of the Ocala group and samples of Claiborne age is less than the
normal thickness of the Ocala group. This indicates that either the
lower part of the Ocala group or the top part of the Claiborne group
is missing in well W-1364. These wells lie along a line striking
northeast. Wells to the northwest and to the southeast of this
line appear to have a normal thickness of the Ocala group.
Wells southeast of the above line have thicker sections of the
Suwannee limestone and the Tampa formation than wells northwest
of the line. The displacement necessary to account for the ob-
served thicknesses can be seen on sections A-A' and B-B' (Plates
III and IV). No evidence for thinning caused by an unconformity
could be detected.
A normal fault dipping steeply to the southeast explains best
the thin Ocala group sections along the fault and the thick Suwannee
limestone and Tampa formation sections southeast of the fault.
The Cypress fault is of post-Suwannee-pre-Tampa age. There is
some indication that movement may have continued into early Mio-
cene time while the Tampa formation was being deposited. The
Tampa formation is gently folded in Calhoun County south of
Jackson County in the zone where the steeper dips, caused by drag
near the fault, are returning to the more gentle regional dip (figure
13).
The structure maps of the top of the Ocala group and the Clai-
borne, (figures 5 and 6) and the structure sections A-A' and B-B'
(Plates III and IV) show the details of the fault as they are known.
The dip of the fault cannot be determined with certainty, but it must


2Please refer to the Letter of Transmittal














STRUCTURE MAP

OF THE

CLAIBORNE EOCENE
All doae fr wel itudl i
Contw datum meon 1U 1vel
--.IS. CONTOUR DOTTED WHERE UNCERTAIN
O WELL SAMPLE
X SURFACE OUTCROP
___ PROBABLE PRE TAMPA POST SUWANNEE FAULT

SCALE


w n a w I R 5 W I R 4 W WU


Figure 5.-Structure map of the Claiborne Eocene.


a 14 R I w iw r


"


. . . I D













STRUCTURE MAP
OF THE
OCALA GROUP
Contour dam m.on i.e I.vl
-.6O- CONTOUR OOTTEO WHERE UNCERTAIN
IUAA r LIMIT OF OUTCROP
0 WELL SAMPLE
x SURFACE OUTCROP
PROBABLE PRE TAMPA POST SUNWANEE FAULT

SCALE
4 0 4 ----1254


R 14 w I R is I R .i I R I


S I r t I I r I R 7 I I R W I 4 I

Figure 6.-Structure map of the Ocala group





GEOLOGY OF JACKSON COUNTY, FLORIDA


dip steeply to the southeast. It is reported that the oil test well
W-2777, drilled to the east of the fault, did not encounter the fault,
but it was located almost a mile east of the fault and was drilled to
a depth of only 4113 feet. If the dip of the fault is as much as 45
degrees, well W-2777 would not have encountered the fault at the
total depth reached.
The throw of the fault varies along the strike as shown on the
Ocala group structure map (figure 6). The throw is greater south-
west of the nose shown on the structure map than it is to the north-
east of the nose.
The downthrown block of the fault southeast of the fault trace
seems to have acted as a structurally negative unit prior to the last
recognizable movement. A distinctly deeper water biofacies of the
Ocala group exists southeast of the fault than that found to the
northwest. Further, the Tallahassee and the Avon Park limestones
of middle Eocene age are missing in Jackson County, but they are
present in Gadsden County to the southeast.
The thicker Oligocene section southeast of the Cypress fault
resulted from nondeposition or erosion of the Suwannee limestone
on the upthrown block to the northwest of the fault during faulting
and prior to deposition of the Tampa formation. The slightly
thicker section of Tampa formation on the downthrown block is
further indication that movement associated with the faulting con-
tinued into Tampa time.
OCALA GROUP
History.-The literature pertaining to the "Ocala limestone" is
extensive, has been adequately reviewed in previous publications,
and need not be repeated here. Excellent summaries are contained
in Florida Geological Survey Bulletins 21 and 29. Applin and Applin
(1944 pp. 1683-1685) divided the "Ocala limestone" into an upper
and a lower member, but stated that "In west Florida where the
Ocala is chiefly cream-colored chalk, it is not possible at present to
recognize the two members seen in the peninsular area." Vernon
(1951, p. 111) subdivided the "Ocala limestone" into the "Ocala
limestone (restricted)" and the Moodys Branch formation, the
latter of which he divided into the Williston and Inglis members.
Puri (1953, p. 34), in a paper presented before the Society of Eco-
nomic Paleontologists and Mineralogists used the term Ocala group
and divided the Ocala group into three formations: the Crystal
River formation, the Williston formation, and Inglis formation.
The Williston and Inglis formations are Vernon's members of





FLORIDA GEOLOGICAL SURVEY


the Moodys Branch formation raised to formational rank. The
Crystal River formation for the most part is equivalent to the
"upper Ocala" of Applin and Applin.
Beds younger than the Crystal River of Puri occur in Jackson
County at the top of the Ocala Group. These beds are here named
the Bumpnose limestone member of the Crystal River limestone
for the exposures along and near the Bumpnose road north and
west of Marianna, Florida. Further, there is present in the sub-
surface of southeastern Jackson County a series of beds of Crystal
River age that thicken to the southeast and are characterized by
a deeper water foraminferal fauna. The fauna and lithology of
this unit is so distinctive that it should be given a distinguishing
name. The name Gadsden limestone is proposed for this deeper
water facies of Crystal River age because the fauna and lithology
of the unit was first described by Cole (1944) from the samples
of the City of Quincy water well, W-4, in Gadsden County.
As already noted, the Moodys Branch formation appears to be
absent in Jackson County. This would indicate that the Jackson
County section is minus the lower part of the Ocala Group (Moodys
Branch equivalents) or that the lower portion cannot be distin-
guished from the upper portion, and that it includes beds younger
than those exposed at Crystal River. Because the Bumpnose lime-
stone is equivalent to the youngest Eocene known in the Carib-
bean region, a combination of the sections in Jackson County and
those of the peninsular area of Florida include a complete Jackson
Eocene sequence. It should be pointed out, however, that the Jack-
son County section and the Citrus and Levy county sections of the
Crystal River are separated in the subsurface by the Gadsden lime-
stone so that the Crystal River cannot be traced directly from the
Peninsular area to the Jackson County area.
In this report the term Crystal River will be used to refer to all
of the Crystal River in Jackson County except where the Bumpnose
limestone member is referred to by its own member designation.
The Bumpnose limestone is considered to be a member of the
Crystal River formation, although it is younger than the youngest
Crystal River exposed at the type locality. A member designation
was chosen for the Bumpnose limestone rather than a formational
designation because of the limited geographic extent of the unit.

CRYSTAL RIVER FORMATION
Historical.-Florida Geological Survey Bulletins 21 and 29
should be consulted for more complete summaries of the earlier




GEOLOGY OF JACKSON COUNTY, FLORIDA


work with the Ocala group ("Ocala limestone"). Applin and Applin
(1944, p. 1683) divided the "Ocala limestone" into an upper and a
lower member, Vernon (1951, p. 111.) subdivided the "Ocala lime-
stone" into two formations, the "Ocala limestone (restricted)" and
the Moodys Branch formation. He subdivided the Moodys Branch
formation into a lower member, the Inglis, and an upper member,
the Williston. Puri (1953, p. 34) used the term Ocala group and de-
fined some of the units to be included in the Ocala Group. Puri pro-
posed the name Crystal River formation for Vernon's "Ocala (re-
stricted)" and raised Vernon's Inglis and Williston members to
formation rank.

In his study of the Oligocene stratigraphy of the Southeastern
United States, MacNeil (1944, pp. 1324-1325) questioned the
Jackson age assigned to the Lepidocyclina (Nephrolepidina) chaperi
Lemoine and R. Douvill6 zone (=L. (N.) fragilis Cushman). This
zone is the Bumpnose limestone member of this report. MacNeil
found associated with L. (N.) chaperi the following species:
Clypeaster sp., Pecten anatipes, and Spondylus dumosus, which
farther west in Alabama and Mississippi appear in unquestioned
Oligocene sediments. MacNeil correlates the L. (N.) chaperi zone
with the Red Bluff clay of Mississippi. In this report the L. (N.)
chaperi zone is considered to be of Jackson age, but it is treated as
a separate member of the Crystal River limestone, the Bumpnose
limestone member.

Definition.-The Crystal River formation of this report includes
all limestones containing Jackson Eocene orbitoid and camerinid
faunas that underlie the Marianna limestone or younger beds and
overlie the beds of Cook Mountain (lower middle Eocene) age with
Operculinoides sabinensis. The Bumpnose limestone member of
the Crystal River formation includes those soft, white, limestones
characterized by Lepidocyclina (Nephrolepidina) chaperi and over-
lain by the Marianna limestone with L. (Lepidocyclina) mantelli
and underlain by the harder cream-colored Crystal River limestone
bearing Operculinoides ocalanus, Operculina mariannensis, and
Asterocyclina spp.

Lithology.-The Crystal River formation is a white to cream-
colored, generally soft, granular, permeable, fossiliferous, pure
limestone. It is frequently composed almost wholly of the tests of
orbitoidal Foraminifera and Bryozoa. Frequently it has been
hardened by recrystallization to a dense limestone, and locally the




FLORIDA GEOLOGICAL SURVEY


exposed surface of the formation may be silicified, taking on a pink-
ish or brownish color.

The Bumpnose member is normally softer and whiter than the
Crystal River and is slightly glauconitic. The abundance of large
specimens of L. (N.) chaperi is a characteristic of the lithology of
the Bumpnose member.

Thickness and Structure.-Within Jackson County the Crystal
River formation has a thickness of about 220 feet including the
Bumpnose member. The top of the formation used in constructing
the structure map (Figure 6) is placed at the first appearance of
a Jackson Eocene fauna in the wells studied for this report. A
thin Ocala group section was observed in well W-1356, W-1358, and
possibly W-1364. A normal fault dipping to the southeast is
believed to explain best the observed thicknesses (see p. 26).

The structure of the Crystal River formation can be illustrated
best in sections, plates III, IV, and V (vertical scales exaggerated),
and by a structural map, figure 6. Regionally the Crystal River
formation dips southeast in the eastern part of the county and
south in the central and western parts of the county.

Paleontology.-The Crystal River formation, excluding the
Bumpnose member, is characterized by: Operculinoides ocalanus
(Cushman), Operculina mariannensis Vaughan, Asterocyclina spp.,
Pseudophragmina (Proporocyclina) citrensis (Vaughan), Lepi-
docyclina (Lepidocyclina) montgomeriensis Cole, L. (L.) ocalana
Cushman, and Amusium ocalanum Dall. Many species of echinoids
(Cooke, 1941, 1942) and mollusks are common. A check list of the
Foraminifera identified from various localities and wells in Jackson
County is given in Table 2. The fauna that is characteristic of the
Bumpnose member is listed under the discussion of that member,
and is not included here.

Local Details.-The Crystal River formation lies at or near the
surface over most of the northern half of Jackson County from
about three miles north of Marianna northward to the Alabama
Florida state line (Plate I). Outcrops of the Crystal River forma-
tion are scattered because of a veneer of terrace deposits. This area
has less relief than the southern half of the county where the more
impermeable Marianna limestone, the clayey phase of the Suwannee
limestone, and the clays of the Tampa formation crop out.




GEOLOGY OF JACKSON COUNTY, FLORIDA 33

Crystal River Gadsden
Formation Limestone
TABLE 2 Lower
TYPICAL OCALA GROUP Member
FORAMINIFERAL FAUNAS Bumpnose -5, J-156,
Member J-139, W-1987,
.-5 W-1824 278'-288'
Amphistegina alabamensis Applin & Jordan X X
Asterocyclina georgiana (Cushman) X
Asterocyclina nassauensis Cole X
Angulogerina byramensis (Cushman) X
Angulogerina vicksburgensis Cushman X
Anomalina bilateralis Cushman X X
Bolivina cf B. jacksonensis Cushman & Applin X X
Bolivina paula Cushman & Cahill X
Bolivina caelata Cushman X X
Bolivina byramensis Cushman X
Bolivina striatellata Bandy X
Bulimina ovata d'Orbigny X
Camerina vanderstocki (M. Rutten
& Vermunt) X
Cibicides mississippiensis (Cushman) X
Cibicides pippeni Cushman & Garrett X X
Cibicides pseudoungeriana (Cushman) X
Dentalina jacksonensis (Cushman & Applin) X
Dentalina cf. D. soluta Reuss X
Dentalina vertebralis (Batsch) X
Eponides jacksonensis (Cushman & Applin)
var. X X
Eponides cf. E. ocalanus Cushman X
Eponides cf. E. rutteni Cushman &
Bermudez, var. X
Gaudryina sp. X
Gaudryina gardnerae Cushman X
Globigerina spp. X X X
Globorotalia cocoanensis Cushman X
Guttulina byramensis (Cushman) X
Guttulina gibba d'Orbigny X X
Guttulina irregularis (d'Orbigny) X
Guttulina problema d'Orbigny X
Gypsina globula (Reuss) X X
Gyroidina sp. X
Gyroidina obesa Bandy X
Helicolepidina spiralis Tobler X
Liebusella byramensis turgida (Cushman) X
Lepidocyclina (Lepidocyclina) montgomeriensis
Cole X X
Lepidocyclina (Lepidocyclina) ocalana
Cushman X X
Lepidocyclina (Lepidocyclina) ocalana
floridana Cushman X





FLORIDA GEOLOGICAL SURVEY


Crystal River Gadsden
Formation Limestone
TABLE 2 (Continued) Lower
Member
TYPICAL OCALA GROUP Bumpnose J-5, J-156,
FORAMINIFERAL FAUNAS Member J-139, W-1987,
J-5 W-1824 278'-288'
Lepidocyclina (Nephrolepidina) chaperi
Lemoine & R. Douvill X
Lingulina sp. X
Marginulina cocoaensis Cushman X
Marginulina cf. M. digitalis Bandy X
Nodosaria cf. N. cookei Cushman X
Nodosaria fissicostata (Giimbel) X
Nodosaria latejugata Giimbel X
Operculina mariannensis Vaughan X
Operculinoides jacksonensis (Gravell &
Hanna) X
Operculinoides ocalanus (Cushman) X
Planorbulina larvata X
Planulina cf. P. cocoaensis Cushman X X
Pseudophragmina (Proporocyclina)
citrensis (Vaughan) X
Pyrgo inornata (d'Orbigny) X
Reussella eocena (Cushman) X
Robulus spp. X X
Robulus cocoaensis (Cushman) X
Robulus inusitatus Cushman X
Robulus limbosus (Reuss) X
Siphonina advena Cushman X X
Siphonina jacksonensis Cushman & Applin X
Textularia distinct (Cushman) X
Textularia mississippiensis Cushman X
Textularia seligi Stucky X
Uvigerina cocoaensis Cushman X
Uvigerina cookei Cushman X
Uvigerina dumblei Cushman & Applin X
Uvigerina glabrans Cushman X X
Uvigerina jacksonensis Cushman X
Valvulineria octocamerata (Cushman &
Hanna) X X

Loc. J-2, a sink hole, in the center of the E 1l/ NE 1/4 sec. 31,
T. 6 N., R. 9 W. exposes 12 feet of upper Crystal River formation.
The elevation of the land surface at the side of the sink is about 125
feet. Only a small amount of overburden is present.
Loc. J-5, a quarry, figure 7, near the center W 1/. sec. 23, T. 5 N.,
R. 11 W. exposes approximately 2 feet of Crystal River formation
at the bottom of the pit in the floor of the north quarry with
Amusium ocalanum and Asterocyclina sp. Near the bottom of the




GEOLOGY OF JACKSON COUNTY, FLORIDA


small pit in the floor of the north quarry, the Crystal River forma-
tion is overlain by approximately 15 feet of the Bumpnose member.
This is probably the best locality in Jackson County to study the
relationships between the Crystal River formation, the Bumpnose
member, and the Marianna limestone.
Loc. J-11, an abandoned quarry, at the road corner in the SE
1/4 SW 1/4 sec. 29, T. 6 N., R. 11 W. exposes approximately 15 feet
of the Asterocyclina zone of the Crystal River formation. Echinoids
are abundant in this quarry.
Loc. J-12, an abandoned quarry, just east of the highway (Fla.
75-U.S. 231) in the SE 1/ sec. 13, T. 6 N., R. 12 W. exposes about
15 feet of the uppermost Crystal River overlain by 5 feet of hard
limestone of the Bumpnose member. Figure 8 shows the discon-
formity between the lower portion of the Crystal River formation
and the Bumpnose member. MacNeil (1944, p. 1325) refers the
upper bed to the L. (N.) chaperi zone. Cooke (1945, p. 67) listed
a large thick Lepidocyclina sp., Pecten poulsoni, Clypeaster sp.
(probably C. rogersi) from this bed and regarded it as an unmapped
outlier of the Marianna limestone. Cooke does not now include the
L. (N.) chaperi zone in the Marianna limestone.1
Loc. J-138, a sinkhole, just north of the road in the southeast
corner of the SW 1/4 sec. 23, T. 6 N., R. 9 W. exposes 8 feet of hard
crystalline limestone that contains Amusium ocalanum of Crystal
River age. The elevation of the land surface at the top of the sink
in 128 feet. This limestone trends generally north-south and the
outcrop has a width of about 50 feet.
Loc. J-139, a deep sinkhole, on the west side of the road at NE
1/4 NE 1/ sec. 21, T. 6 N., R. 9 W. exposes 27 feet of the Asterocy-
clina zone of the Crystal River formation. The elevation at the top
of the sink is 130 feet. This is an excellent exposure of the Crystal
River formation and is very fossiliferous.
Loc. J-150, a sinkhole, in a field in the NW 1/ NW 1/4 sec. 10, T. 5
N., R. 9 W. exposes about seven feet of Crystal River formation over-
lain by 3 feet of mantle. The elevation of the land surface at the
top of the sink is 112 feet.
Loc. J-156, an abandoned quarry, north of Waddell's Mill Pond
in the NE 1/ SE 1/ sec. 32, T. 6 N., R. 11 W. exposes about 35 feet
of the Asterocyclina zone of the Crystal River formation. The ele-


1Personal communication.




FLORIDA GEOLOGICAL SURVEY


vation of the top of the limestone is estimated to be 120-130 feet.
In the upper 20 feet Asterocyclina sp. is very abundant. The check-
list (table 2) includes species that have been identified from this
locality. This is one of the best Crystal River formation exposures
in Jackson County (Stop No. 8, Southeastern Geological Society,
Third Field Trip, Western Florida, p. 18, Nov. 9, 10, 1945).

Loc. J-157, a sinkhole, on the south side of the road, SW 1/4 NE
1/4 sec. 36, T. 6 N., R. 9 W., exposes 9 feet of the Asterocyclina zone
of the Crystal River formation. The elevation of the top of the sink-
hole is about 130 feet.

Loc. J-185, a bluff, on the west side of the Chipola River flood-
plain SE 1/4 sec. 28, T. 5 N., R. 10 W. exposes the Asterocyclina zone
of the Crystal River formation. Asterocyclina spp. occur just above
the level of the floodplain.
Thirty-five wells that reached the Crystal River formation are
listed in Appendix I, where the depth at which the formation was
encountered is indicated.

Bumpnose Member of the Crystal River formation
Historical.-The limestone herein called the Bumpnose was first
included in a section published by Cooke (1915, p. 109). The details
of Cooke's section follow:

"Section 200 yards below the wagon bridge east of
Marianna, Fla.
Marianna limestone: Feet
5. White limestone, the same as bed No. 5
of the section at the bridge ------ 33
Ocala limestone:
4. Soft cream-colored limestone with several
species of Orbitoides and some Bryozoa ..--- 1
3. Hard semicrystalline pinkish limestone
with large Orbitoides, Flabellum and
Amnusium ocalanum ____----------- 61/2
2. Soft granular cream-colored limestone
like No. 1 of section at bridge but with
fewer Foraminifera. Contains Orbitoides
(stellately marked species), Flabellum,
Bryozoa, Terebratulina lachryma?, Nati-
ca, Arca, Pecten indecisus, Amusium
ocalanum and Plicatula (Ocala species) --.- 3
1. Concealed to water level in Chipola River 3"

Cushman (1920, pp. 63-64) described Lepidocyclina fragilis
[L. (Nephrolepidina) chaperi of this report] from bed four of the
above section. As Cooke considered this bed to be Ocala in age,
L. (N.) chaperi was thought to be a marker for the upper "Ocala





GEOLOGY OF JACKSON COUNTY, FLORIDA


limestone." The age of this zone was not questioned until MacNeil
(1944, p. 1324) found species associated with L. (N.) chaperi which
farther west appear to be confined to the Oligocene. MacNeil cor-
related this horizon with the Red Bluff clay of Alabama and Mis-
sissippi.
Cole (1945, pp. 17-19) reported Lepidocyclina (Nephrolepidina)
sanfernandensis Vaughan and Cole, var. tallahasseensis Cole and
Helicolepidina paucispira Barker and Grimsdale from the bottom
of the City of Tallahassee water well, W-453. Helicolepidina pau-
cispira at that time was known to occur only at the base of the upper
Eocene in Mexico (Barker and Grimsdale, 1936, pp. 243, 247). L.
(N.) sanfernandensis was known only from the type locality at San
Fernando, in Trinidad, in deposits considered to be of late Eocene
age. As this fauna was not typical of any known locality in the
"Ocala limestone," Cole referred that portion of the well to the
upper Eocene without a specific formational designation. Cole
(1952, pp. 23-27) has shown that L. (N.) fragilis and L. (N.) san-
fernandensis var. tallahasseensis are synonyms of L. (N.) chaperi.
At locality J-5 in Jackson County, Florida, (fig. 7) specimens of
Helicolepidina spiralis Tobler were found in association with Lepi-
docyclina (Nephrolepidina) chaperi Lemoine and R. Douvill6, Lepi-


Srj .k 'L
..w


4* -,~ ...
j M
r'vio


Figure 7.-Locality J-5, Marianna Limestone Products Co. Rock being
quarried is Lepidocyclina (Nephrolepidina) chaperi zone, the Bumpnose mem-
ber, and the Crystal River formation.





FLORIDA GEOLOGICAL SURVEY


docyclina (Lepidocyclina) montgomeriensis Cole, L. (L.) georgiana
Cushman, and L. (L.) ocalana Cushman. Further, the matrix
around a nautiloid specimen, Aturia alabamensis, which came from
the uppermost part of the Bumpnose limestone at this locality,
contained specimens of Helicolepidina spiralis, L. (L.) montgomer-
iensis, and L. (N.) chaperi. The faunal checklist (table 2) indi-
cates the various species which have been found in the Bumpnose
limestone.
The late Professor G. D. Harris and Dr. K. V. W. Palmer kindly
consented to examine the pelecypods and gastropods although pres-
ervation of the latter was so poor that specific identifications were
not possible. Professor Harris' opinion of this pelecypod fauna
is quoted:'
"Our interpretation of your material is that it came from Ocala beds in
which Oligocene species were gradually infiltrated."
When compared with the Crystal River large Foraminifera
fauna immediately underlying the Bumpnose limestone, the fauna
of the Bumpnose limestone indicates a loss of Asterocyclina, Pseudo-
phragmina, and Operculinoides species, the retention of Lepido-
cyclina (Lepidocyclina) montgomeriensis, L. (L.) georgiana, and
L. (L.) ocalana, and the additions of Helicolepidina spiralis, else-
where considered to be restricted to the Eocene, and Lepidocyclina
(Nephrolepidina) chaperi, the first appearance of the subgenus,
but a species which in Panama and elsewhere is associated with
typical Jackson stage Eocene genera and species including Astero-
cyclina species, (Cole, 1952, p. 4). Careful examination revealed
no specimens of previously accepted Oligocene species of large
Foraminifera in the Bumpnose member.
MacNeil (1944, p. 1325) refers the upper limestone member
which unconformably overlies the Crystal River limestone (fig. 8)
in an abandoned quarry (locality J-12 of this report) to the L. (N.)
chaperi zone. Cooke (1945, p. 67) considered this same member to
represent the Marianna limestone.
C. Wythe Cooke (letter, May 1, 1952), after examining two
echinoid species from the Bumpnose limestone at locality J-5, stated:
"The occurrence in this zone of a Clypeaster and Pecten anatipes as
reported by MacNeil is very suggestive of Oligocene age, though I agree
with him that the zone does not belong in the Marianna Limestone. His
suggestion that it should be correlated with the Red Bluff clay, which
is supposed to be early Oligocene, seems very plausible. The known fauna
of the Red Bluff has some Eocene aspects."
tPersonal letter dated November 7, 1950, a copy of which is on file at the
Florida Geological Survey.




GEOLOGY OF JACKSON COUNTY, FLORIDA


Figure 8.-Locality J-12. The uppermost bed is the Lepidocyclina (Nephro-
lepidina) chaperi zone. The lower rock is more typical of the Crystal River
formation.

Cooke reports the two echnoid species as new species of Aniso-
petalus and Clypeaster (closely related to C. rogersi).
It is my opinion that this zone is of uppermost Jackson age,
rather than of Oligocene age as suggested by MacNeil. It must be
recognized, however, that there seems to be an infiltration of Oligo-
cene forms and that this represents a transition between the two
series.
The upper contact of the Bumpnose limestone can be observed
best at locality J-74, where it is conformably overlain by the Mari-
anna limestone. The uppermost part of the Bumpnose limestone is
glauconitic as it is at locality J-5. The base of the Bumpnose lime-
stone can be seen at locality J-5 but quarrying operations tend to
obscure the contact. At locality J-12, however, the base of the
Bumpnose limestone is clearly exposed, and it is slightly unconform-
able (fig. 8) with the underlying Crystal River formation.
The distribution of the Bumpnose limestone in Florida is re-
stricted. It appears to be present at the surface only on the
Marianna-Chipley structural high and in the subsurface in the
Tallahassee area. Wells in Washington County have not been
studied to verify its presence there, but it probably does extend




FLORIDA GEOLOGICAL SURVEY


into Washington County. The Bumpnose limestone was not recog-
nized in well W-1987 at Sink Creek, where a somewhat deeper water
Jacksonian fauna was encountered, but a new species, probably
belonging to the Amphisteginidae, that occurs in the Bumpnose
limestone, was present in the well at the stratigraphic position of
the formation.

This restriction of the Bumpnose limestone to the structurally
higher areas in west Florida, the prolific occurrence of the one
species, L. (N.) chaperi, and the abundant bryozoans of the zone
suggests that this zone represents a distinct biofacies of the upper-
most Jacksonian.

Definition.-The Bumpnose limestone member of this report,
a new name, is the uppermost member of the Crystal River forma-
tion and contains Lepidocyclina (Nephrolepidina) chaperi Lemoine
and R. Douvill&. It occurs above the Asterocyclina zone of the
Crystal River formation and below the Marianna limestone which
contains Lepidocyclina (Lepidocyclina) mantelli (Morton). The
member is named for the many occurrences in the general vicinity
of the Bumpnose road north of Marianna. Locality J-5 is the type
locality for the member.

Lithology.-The Bumpnose limestone is a soft, easily crumbled,
white limestone that is generally more granular than the typical
Marianna limestone because of the presence of many Bryozoa and
Foraminifera. It is generally somewhat glauconitic, especially near
the top of the member.

Thickness.-The thickness of the Bumpnose limestone ranges
from 0 to 15 feet in Jackson County. It apparently thins to the
southeast where it is replaced by the Gadsden limestone southeast of
the Cypress fault.

Paleontology.-The striking and characteristic feature about
the fossils of this horizon is the abundance of specimens of Lepi-
docyclina (Nephrolepidina) chaperi Lemoine and R. Douvill6 with
a virtually bewildering variation in shape. Bryozoa are present
in large numbers and several species are represented. The checklist
(table 2) indicates the species which were determined. A new
amphisteginid species whose affinities are not yet clear appears to
be restricted to this horizon though its areal distribution is greater
than L. (N.) chaperi.





GEOLOGY OF JACKSON COUNTY, FLORIDA


Local Details.-A quarry (loc. J-5) located near the center of
the W 1/2 sec. 23, T. 5 N., R. 11 W. exposes 15 feet of the Bumpnose
limestone. The elevation of the top of this formation is 115 feet.
A small pit located within a larger quarry, is now being mined at
this site. This elevation corresponds with the floor of the large
quarry and the rim of the smaller pit, (fig. 7). This is the best ex-
posure of the Bumpnose limestone in Jackson County since the zone
is overlain by the Marianna limestone and underlain by about 2
feet of Crystal River formation. The following section was mea-
sured at locality J-5 in 1948:

Loc. J-5
Top of quarry face.
Marianna limestone Feet
10. Hard, weathered limestone 2.0
9. Soft, creamy white limestone with scattered
Lepidocyclina (Lepidocyclina) mantelli,
Operculinoides dius, and Pecten. 5.2
8. Hard lenses made up of L. (L.) mantelli 1.0
7. Soft "chimney rock" phase of Marianna ls. 5.4
6. Soft, "chimney rock" matrix with many specimens of
L. (L.) mantelli 2.0
5. Soft, creamy white "chimney rock" as in bed 7 5.4
Unconformity?
Crystal River formation
Bumpnose member
4. Soft to hard, fine to granular white limestone, upper
6 inches glauconitic, becoming less so toward bottom of
member. L. (Nephrolepidina) chaperi and mollusk molds
abundant. Aturia alabamensis collected near top of bed. 5.4
3. Granular, white, very fossiliferous limestone, L. (N.)
chaperi, very abundant with many very large micro-
spheric specimens, and Pecten anatipes. 5.4
2. Harder, creamy white limestone with fossils as in bed 3. 5.4
Unconformity
Lower member of Crystal River formation
1. Hard, buff to cream colored limestone with Amusium
ocalanum. No Lepidocyclina noted. 2.0
Total thickness of section ............ .. ... ------39.2
The checklist (table 2) shows the species which have been identified
from this quarry.

Loc. J-74, a bluff, just northeast of the highway Fla. 73 in the
southeast corner NW 1/4 sec. 25, T. 5 N., R. 11 W. exposes 10 feet
of the Bumpnose limestone. The limestone lying above the Bump-
nose limestone and extending to the top of the bluff is referred to
the Marianna limestone, but the Southeastern Geological Society
(1945, p. 16, Stop. No. 7) referred this to the Byram marl. The
elevation of the top of the bluff is about 135 feet and the elevation
of the contact between the Bumpnose limestone and the Marianna
limestone is 106 feet.





FLORIDA GEOLOGICAL SURVEY


Loc. J-77, a roadside exposure, in the NW 1/4 SE 1/4 sec. 29, T.
5 N., R. 10 W. exposes the contact between the Marianna limestone
and the Bumpnose member. The elevation of the contact, at the
foot of the hill, is 93 feet.
Loc. J-97, a roadside outcrop, at the center of the east side of
the SE 1/ sec. 20, T. 5 N., R. 10 W. exposes an obscure contact be-
tween the uppermost portion of the Bumpnose limestone and the
basal portion of the Marianna limestone. A little over 5 feet of hard
cherty limestone assigned to the Bumpnose limestone is exposed in
the roadbed at the gate to the superintendent's house, Florida
Caverns Park.
Loc. J-149, a sink, in the SW 1/4 NE 1/4 sec. 9, T. 5 N., R. 9 W. ex-
poses 5 feet of the Bumpnose limestone overlain by one or two
feet of mantle rock. The elevation of the land surface at the top
of the sink is 132 feet.
Loc. J-193, a small sinkhole, in a field in the NW 1/4 SE 1/t sec.
15, T. 5 N., R. 9 W. exposes two or three feet of the Bumpnose
limestone. The elevation of the top of the limestone is 116 feet.
The Bumpnose limestone was readily recognizable in wells and
it was logged in the following wells: W-276, W-1356, W-1783, W-
1793, W-1794, W-1824, W-2252, W-2328, W-2415, W-2433, and
W-2531. Appendix I gives the depths at which it was encountered
in each case.
GADSDEN LIMESTONE
Historical.-The Gadsden limestone is a new name introduced
here for some limestones of Jackson age that occur in the subsurface
sections of southeastern Jackson County. These limestones have a
foraminiferal fauna dominated by the families Buliminidae and
Lagenidae. The Foraminifera Lepidocyclina, Asterocyclina, and
Operculinoides are generally absent in the Gadsden limestone.
Dense brown chert is present in the upper part of the Gadsden lime-
stone, and the Gadsden limestone is finer grained than the limestone
of the Crystal River formation because of the absence of the larger
Foraminifera. Well W-4, the City of Quincy water well in Gadsden
County, is designated as the type well, and the interval from 680
feet to at least 900 feet in this well is assigned to the Gadsden lime-
stone. Samples from this well are on file at the Florida Geological
survey. The top of the Gadsden limestone is easily determined in
well W-4 and in most of the wells studied, but, unfortunately, the
bottom of the formation is not so obvious in well W-4. The Applins





GEOLOGY OF JACKSON COUNTY, FLORIDA


(1944, p. 1678) indicate that Eponides aff. cocoaensis is one of the
key fossils for the Tallahassee limestone, which underlies the Gads-
den limestone in well W-4. E. cocoaensis appears at 900 feet in
well W-4, but there is little else to mark the bottom of the Gadsden
limestone, and it may extend deeper than indicated above.
The limestones that are referred to here as the Gadsden lime-
stone were first described by Cole (1944, p. 11-18) from the City
of Quincy water well W-4. Cole applied the name "Ocala" to the
rocks below 680 feet in well W-4, but he noted that the fauna was
not that of the typical "Ocala limestone" elsewhere in Florida, be-
cause it contained no large Foraminifera. Applin and Applin (1944,
p. 1736) accepted Cole's "Ocala" designation for a part of the
Eocene section of well W-4, but they assigned only the interval from
650 feet to 910 feet to the "Ocala." The Applins placed the top of
the "Ocala" thirty feet higher than Cole had placed it, and they as-
signed the lower part of the section, below 910 feet, to the Talla-
hassee limestone. The samples from well W-4 have been examined,
and the top of the Gadsden limestone (="Ocala") is placed at a
depth of 680 feet. The bottom of the Gadsden is placed tentatively
at 900 feet, and it is believed to extend somewhat lower in the well,
but a clearcut bottom for the Gadsden limestone could not be located
in this well. No more than an additional 20 to 30 feet would be in-
cluded in the Gadsden limestone. Not all of the lower part of the
well to the total depth of 1395 feet belongs in the Jackson stage.

Definition.-The Gadsden limestone in Jackson County consists
of those limestones of Jackson age that have no, or few, specimens
of the larger Foraminifera such as Lepidocyclina, Asterocyclina, or
Operculinoides. The Gadsden limestone is known to occur only in
the subsurface at present. The foraminiferal fauna of the Gadsden
limestone is dominated by the families Buliminidae and Lagenidae,
which make up from 40 to 50 percent of the foraminiferal popula-
tion. The Gadsden limestone is overlain in Jackson County by the
Marianna limestone. The Gadsden limestone is the stratigraphic
equivalent of the Crystal River formation, which includes the Bump-
nose member. The Gadsden limestone grades laterally into the Crys-
tal River formation in Jackson County, and the youngest beds of the
Gadsden limestone extend farthest to the northwest (Plate IV). De-
pending upon where the Gadsden limestone is encountered in wells,
it is underlain by the Crystal River formation or by older Eocene
formations. The Tallahassee limestone underlies the Gadsden lime-
stone in well W-4 in Gadsden County.





FLORIDA GEOLOGICAL SURVEY


Lithology.-The Gadsden limestone is a buff to white limestone
that is porous, soft, and fine grained. Near the top of the Gadsden
limestone there is a zone of dense, brown chert that was not noted
in the Crystal River limestone. Selenite occurs in the Gadsden
limestone in well W-4, but none was noted in Jackson County.

Thickness and Structure.-The Gadsden limestone ranges from
0 to 180 feet in thickness in Jackson County. The Gadsden lime-
stone is confined to the area southeast of the Cypress fault, and
from the fault it thickens to the southeast at the expense of the
Crystal River formation, with which it is equivalent. The Gadsden
limestone occurs only on the downthrown side of the Cypress fault,
and aside from the nose, shown on structure map figure 6, the
Gadsden limestone dips to the southeast.

Paleontology.-The Gadsden limestone does not contain the
large Foraminifera that are typical in rocks of Jackson age in
Florida. Instead, it carries a fauna composed primarily of the
foraminiferal families Buliminidae and Lagenidae. The abundance
of Jacksonian species of Uvigerina, Bulimina, Bolivina, Dentalina,
Nodosaria, Marginulina, and Robulus is noteworthy and typical.
These elements of the fauna may constitute 40 to 50 percent of the
total foraminiferal fauna. Table 2 indicates species that have been
identified from the Gadsden limestone.

Local Details.-The Gadsden limestone was encountered in all
wells southeast of the Cypress fault that encountered rocks of
Jackson age. As indicated in Plate IV, the formation thickens to
the southeast at the expense of the Crystal River formation. Ap-
pendix I lists all wells studied that penetrated the Gadsden lime-
stone.
OLIGOCENE SERIES
VICKSBURG GROUP

MARIANNA LIMESTONE
Historical.-Florida Geological Survey Bulletins 21 and 29 con-
tain historical summaries pertaining to the Marianna limestone.

Definition.-The Marianna limestone of this report consists of
the light-colored limestones which carry Lepidocyclina (Lepido-
cyclina) mantelli (Morton), and which are underlain by the Crystal
River limestone or the Gadsden limestone, and which are overlain
by the Suwannee limestone.




GEOLOGY OF JACKSON COUNTY, FLORIDA


Lithology.-The Marianna limestone is always light in color,
ranging from white through cream to light gray. It is slightly
glauconitic, and when this rock has been subjected to alternate wet-
ting and drying, as in a poorly drained quarry, it may have rust
colored specks scattered through it. The Marianna limestone en-
countered in well W-1987 in Sink Creek was especially glauconitic.
The limestone is generally massive and impermeable. The large
Foraminifera which characterize the Marianna limestone may be
virtually the sole constituents of some beds. The Marianna lime-
stone is very soft when fresh, and wood saws are used to cut out
pieces for use as building blocks.

Thickness and Structure.-The Marianna limestone strikes east-
west, where exposed at the surface, with only minor variations
(figure 9). The dip is about 13 feet per mile to the south and
steepens to 64 feet per mile at about the south side of T. 4 N. south
of Marianna. This observation is based upon dips of the Suwannee
limestone measured along the Chipola River north of Sink Creek
and the depth of the Marianna limestone in well W-1987 at Sink
Creek. The steeper dip at Sink Creek probably resulted from
drag associated with the Cypress fault.
The thickness is rather uniform, ranging from at least 25 feet
in well W-1987 at Sink Creek to about 35-40 feet in the outcrop
area.

Paleontology.-The Marianna limestone has an abundant fora-
miniferal fauna. Cole and Ponton (1930, pp. 22-23) reported 58
species and varieties of Foraminifera from the Marianna in their
report but the large Foraminifera, especially Lepidocyclina (Lepi-
docyclina) mantelli (Morton) associated with Operculinoides dius
(Cole and Ponton) remain the best guide to the formation.
Bryozoa are abundant locally and Pecten sp. is found at most
localities.

Local Details.-The Marianna limestone, especially where cov-
ered with either the clayey phase of the Suwannee limestone or Mio-
cene clays, forms an escarpment which extends in an east-west
direction from the vicinity of Blue Springs to Cottondale, Florida.
It is in this area that most good exposures occur. The City of
Marianna is on the top of this escarpment, and excellent outcrops
are to be found especially northeast and northwest of Marianna
along the dissected front of the escarpment (Plate 1). The dense,












STRUCTURE MAP

OF THE
MARIANNA LIMESTONE
cAntou dTSM mao s*e Ilerl
--t0O- COTTOUR TTED WHERE UNfRTAIN
.A.A LWIMT OF OUTCROP
0 WELL SAMPLE
X SURFACE OUTCROP
-- PROBABLE PRE.TAMPA POST SUWANNEE FAULT

SCALE

Z- '; -2,I,


I R 7 I 1 6 I T t T A 4 I R 3 W


Figure 9.-Structure map of the Marianna limestone.


w j R F2 W I N D W R
S-


R sa w ( R a3


- -- I o n





GEOLOGY OF JACKSON COUNTY, FLORIDA


massive character of the "chimney rock" facies of the Marianna
limestone tends to make it impermeable to the general percolation
of water through the rocks so that it reacts as a resistant unit,
especially where overlain by impervious clays. The Marianna lime-
stone was identified in the subsurface as far south as Sink Creek
from well cuttings.
Loc. J-189, a sinkhole on the south side of the road in the NE 1/4
NW 1/4 sec. 22, T. 5 N., R. 9 W., exposes 6 feet of badly weathered
Marianna limestone. The elevation of the road alongside the sink
is 115 feet.
Loc. J-1, a chimney rock quarry west of the highway (Fla. 71)
in the NW 1/ NW 1/, sec. 30, T. 5 N., R. 9 W., exposes 19 feet of
the chimney rock phase of the Marianna limestone, overlain by one
to five feet of red residual soil.
Loc. J-78, a road cut, on highway Florida 164 in the approximate
center of sec. 32, T. 5 N., R. 9 W. shows the Marianna limestone-
Suwannee limestone contact. About five feet of Marianna limestone
is overlain by three or four feet of tan, clayey, dolomitic limestone
(figure 10). The elevation of this Marianna limestone-Suwannee
limestone contact is 127 feet.





















Figure 10.-Suwannee limestone at locality J-78 is overlain by "bentonitic"
clays and terrace deposits. The dark halo surrounding the white rock is the
"bentonitic" clay. The Marianna limestone at this locality is not shown in
this picture.





FLORIDA GEOLOGICAL SURVEY


Loc. J-79. At Blue Spring, near the center of the W 1/2 sec. 33, T.
5 N., R. 9 W., 29 feet of Marianna limestone is exposed from the
spring to the top of the hill. The elevation of the water at the spring
is 82 feet. The underground channel from which the spring emerges
is probably in the Bumpnose limestone.
Loc. J-190, a deep sinkhole at the north edge of the road in the
NW 1/4 NW 1/4 sec. 35, T. 5 N., R. 9 W., exposes 20 feet of Marianna
limestone.
Loc. J-14, a road cut on highway U. S. 90 immediately west of
the Chipola River bridge, exposes 19 feet of Marianna limestone
(figure 11). Cooke (1945, p. 80) published the following general-
ized section for this immediate area.
Section on Chipola River at Marianna Feet
3. Byram limestone (Oligocene): finely granular crystalline
limestone like that exposed along Chipola River south of
Marianna. Pecten aff. P. poulsoni and impressions resem-
bling Lepidocyclina supera. Exposed in the cut on High-
way 90. About .-...______--------_____.. -------- 3
2. Marianna limestone (Oligocene) : Massive, homogeneous
white chalky limestone containing Lepidocyclina mantelli
and Pecten poulsoni About ... .....--------- --- 30
Unconformity
1. Ocala limestone (Eocene) : Soft granular white limestone
with hard ledges in upper part. Composed chiefly of cal-
careous organisms locally cemented, including Flabellum
sp., Terebratulina lachryma?, Amusium ocalanum, Plica-
tula sp., and the larger Foraminifera listed on page 67.
Lepidocyclina fragilis at the top to water level, About .---- --- 14


Figure 11.-Locality J-14. Marianna limestone
east of Marianna on highway U. S. 90.


at Chipola River bridge




GEOLOGY OF JACKSON COUNTY, FLORIDA


The upper 12 feet of bed 1 of the above section is the Bumpnose
member of this report and the lower 2 feet of bed 1 is the lower
member of the Crystal River limestone.
The Marianna limestone crops out along the Chipola River as
far south as the SW 1/4 sec. 14, T. 4 N., R. 10 W. There is an abon-
doned chimney rock quarry (J-19) on the west bank of the river
where the L & N railroad bridge crosses the Chipola River near the
center Sl/2 NE 1/4 sec. 10, T. 4 N., R. 10 W.
A number of good exposures of the Marianna limestone and
the overlying Suwannee limestone can be seen along the graded
road north from the western edge of Marianna. One good section
is locality J-76, near the center W 1/2 SE 1/4 sec. 29, T. 5 N., R. 10
W., elevation 122 feet.
The Marjax Co. has a new quarry located in the NW 1/4 SW 1/4
sec. 30, T. 5 N., R. 10 W., not shown on the map, that exposes 12
feet of the Marianna limestone. This quarry was opened after the
field work was completed, and it was not visited.
Loc. J-13, a roadside cut, two miles north of Marianna, measured
from the junction of Florida 167-U. S. 90 on Fla. 167, exposes 28
feet of Marianna limestone overlain by about 16 feet of Suwannee
limestone. The elevation of the Marianna-Suwannee limestone con-
tact is 113 feet. MacNeil (1944, p. 1331) and the Southeastern
Geological Society (1945, p. 19) published sections from this locality,
the best for study of the overlying clayey beds of the Suwannee
limestone (figure 12).
Loc. J-74. A roadside exposure on the north side of the highway
(Fla. 73) in about SE corner NW 1/ sec. 25, T. 5 N., R. 11 W. ex-
poses about 5 feet of Marianna limestone. The elevation of this
roadside exposure is 116 feet. In the woods to the northeast of the
road, a bluff, that cannot be seen from the road exposes about 40
feet of white limestone. The upper 30 feet of this section is re-
ferred to the Marianna limestone, the lower 10 feet is the Bumpnose
member. The elevation of the top of the bluff and top of the lime-
stone is 135 feet. This locality is Stop No. 7 of the Southeastern
Geological Society, Third Field Trip, (1945, p. 16).
Loc. J-5. Two limestone quarries, owned by the Marianna
limestone Products Co., near the center W 1/ sec. 23, T. 5 N., R.
11 W., expose about 40 feet of Marianna limestone overlying the
L. (N.) chaperi zone. The elevation of the top of the Marianna
limestone in the south quarry is 157 feet. A measured section at





FLORIDA GEOLOGICAL SURVEY





Figure 12.-Locality J-13. Marianna limestone overlain by Suwannee
limestone.
the north quarry is to be found on p. 41 of this report. As stated
before, this locality shows the relationships between the Marianna
limestone and the Bumpnose member very clearly.
Several exposures of Marianna limestone are to be found
on a little traveled dirt road running east-west parallel to U. S.
90 and lying about one and one-half miles north. Loc. J-173, a
roadside exposure at the center of the east side of the NE 14 sec.
27, T. 5 N., R. 11 W., exposes about 5 feet of Marianna limestone
overlain by 5 feet of what is believed to be Suwannee limestone.
The elevation of the contact between the two beds is 137 feet. Loc.
J-174, a road cut at about the center of the NE 1/4 sec. 27, T. 5 N., R.
11 W., exposes 20 feet of Marianna limestone overlain by 2 feet of
what is believed to be Suwannee limestone. The elevation of the top
of the limestone in this section is 137 feet.
Loc. J-86, on the side of a hill just north of the L & N railroad
tracks at the southwest corner of the NW 1/ NW 1/ sec. 32, T. 5
N., R. 11 W., 15 feet of Marianna limestone is exposed. The eleva-
tion at the top of the Marianna limestone is 136 feet. A well W-1783,
at the top of the hill just north from this locality encountered the
Marianna limestone at essentially the same elevation. The Marianna
limestone is apparently 40 feet thick at this point (W-1783).


--- 140ft Blow




GEOLOGY OF JACKSON COUNTY, FLORIDA


The following wells penetrated the Marianna limestone: W-l,
W-4, W-276, W-1356, W-1357, W-1358, W-1359, W-1360,
W-1361, W-1362, W-1363, W-1364, W-1783, W-1793, W-1794,
W-1824, W-1987, W-2252, W-2328, W-2329, W-2373, W-2415,
W-2433, and W-2531. Appendix I gives the depth at which the
formation was encountered.

VICKSBURG GROUP AND CHICKASAWHAY MARL
SUWANNEE LIMESTONE
Historical.-Excellent historical summaries relating to the
Suwannee limestone are to be found in Florida Geological Survey
Bulletins 21 and 29. MacNeil (1944, p. 1313-1314, footnote 3)
considered the Suwannee limestone of western Florida to be the
equivalent of the Byram and Chickasawhay formations com-
bined.

Definition.-The Suwannee limestone, as exposed in Jackson
County, consists of tan to buff-colored limestones, dolomitic lime-
stones, and dolomitic to calcareous clays that underlie the greenish-
gray to white Tampa formation. The Marianna limestone under-
lies the Suwannee limestone.

Thickness and Structure. The Suwannee limestone in Jackson
County was subjected to erosion before Miocene deposition began
so that its thickness ranges from 5 to 12 feet in the central area
of the County near Marianna and Cottondale to a maximum thick-
ness in a water well, W-1987, at Sink Creek of about 210 feet.
The Suwannee limestone and the underlying sediments were
gently flexed and faulted during the interval between the Oligocene
and the Miocene, though there is some evidence along the Chipola
River in Calhoun County to the south that this movement may have
continued for some time into the Miocene (figure 13, Plate III).
North of the Sink Creek bridge across the Chipola River the dip
of the Suwannee beds can be observed (figure 14). It is necessary
to use the measured dip of these beds, 64 feet per mile, in construc-
ting a structure section if the observed thickness of the Suwannee
limestone in W-1987 at Sink Creek is to be reconciled with the cal-
culated dip of 12-15 feet per mile on the top of the Marianna lime-
stone in the vicinity of the town of Marianna, (Plate III, see p.
45). South from Sink Creek the dip must lessen once more to
about the regional dip in order to correlate with the section found
in the oil test well, W-7, near Clarksville. That such a flexure has
occurred is further indicated by the rectangular stream course of






FLORIDA GEOLOGICAL SURVEY


Figure 13.-One of a series of gentle arches in the Tampa formation just
south of Jackson County in Calhoun County on the Chipola River. North is
to the right in the picture.


_.,
4 ... ,, '-- --




Figure 14.-Dip of Suwannee limestone at Sink Creek bridge on the Chip-
ola River.




GEOLOGY OF JACKSON COUNTY, FLORIDA


the Chipola River, probably caused by jointing, north of Sink
Creek in the S 1/2 sec. 2, sec. 11, sec. 12, and the N 1/2 sec. 13, T. 3.
N., R. 10 W. This rectangular stream course is best seen on air-
plane photographs, and figure 2 is traced from the aerial photo-
graph mosaic of the U. S. Department of Agriculture photographs
of Jackson County. In sec. 19, T. 2 N., R. 9 W. in Calhoun County
the Chipola River again assumes a more tortuous course than is
normal and small arches of the Tampa formation can be observed
along the river, figure 13.
The nature of the structure of the Suwannee limestone is un-
known in the southwestern part of the country. A few samples
from a well at Compass Lake contained two consecutive samples
which straddled the Suwannee-Tampa contact. Reports from var-
ious water well drillers regarding the top of the "rocks" in wells
along the highway from Compass Lake to Cottondale confirmed
field observations that the top of the Oligocene had been eroded.
The Oligocene-Tampa contact appears to be along an unconformity
in this area (Structure Section, Plate V). The thickness of the
Suwannee limestone in the southwestern part of the county is
unknown. A well at the Florida State Hospital farm, W-276, in
the eastern part of the county shows 115 feet of Suwannee lime-
stone. Figure 15 shows the configuration of the surface of the
Oligocene limestone, usually the top of the Suwannee limestone.

Paleontology.-Table 3 shows the faunas determined for the
Suwannee limestone at various localities and wells.















TOP OF
OLIGOCENE SEDIMENTS
Contour dAolun .Nn s.. level
-'Io- CONTOUR OOTTEL WHERE UNCERTAIN
UIJU4 LIMIT OF OUTCROP
o WELL SAMPLE
X SURFACE OUTCROP
- PROBABLE PRE.TAMPA POST SUWANNEE FAULT

SCALE
4 4 2Mi


R 4 I iFigure 15 I I RO R 9 tp of O cene sedme

Figure 15.-Map, top of Oligocene sediments.


W I R 3 W


- - ^ r I D r u





GEOLOGY OF JACKSON COUNTY, FLORIDA 55

TABLE 3
SUWANNEE LIMESTONE FORAMINIFERAL CHECKLIST

J-32 W-1987 W-2251 W-2194
Textularia mississippiensis Cushman X
Robulus cultrata d'Orbigny X
Robulus gutticostatus d'Orbigny X
Robulus rotulata (Lamarck) d'Orbigny X
Marginulina fragaria (Giimbel) X
Marginulina mexicana Cushman X
Dentalina communis (d'Orbigny) X
Dentalina cocoaensis (Cushman) X
Dentalina jacksonensis (Cushman and
Applin) X
Nodosaria cookei Cushman X
Nodosaria latejugata Giimbel X
Saracinaria italica Defrance X
Guttulina irregularis d'Orbigny X
Nonion umbilicatulum (Montagu) X
Operculinoides antiguensis Vaughan and
Cole X X X
Heterostegina texana Gravell and Hanna X
Bolivina ariana Cole X
Bolivina byramensis Cushman X
Uvigerina gallowayi Cushman X
Eponides mariannensis (Cushman) X
Siphonina advena Cushman X
Cibicides lobatulus (Walker and Jacob) X
Cibicides pseudoungeriana (Cushman) X
Lepidocyclina (Lepidocyclina) asterodisca
Nuttall X
Lepidocyclina (Lepidocyclina) parvula
Cushman X X X X
Lepidocyclina (Eulepidina) undosa
Cushman X X X X


Local Details.-Exposures of Suwannee limestone in Jackson
County are not abundant. The formation is overlain unconform-
ably in much of the county by sandy clays, clays, and marls which
are considered to be lower Miocene in age. An almost continuous
section of the Suwannee limestone is exposed along the Chipola
River south of Marianna.

Oligocene beds are exposed along Rhabb's valley southeast of
Cottondale. Small outcrops are to be found at scattered points south
of a line through Marianna and Cottondale and north of Dry Creek.
In the southeastern part of the county, terrace deposits and the
Tampa formation appear to overlap completely the Suwannee lime-
stone.

At the following localities exposures of the Suwannee limestone
may be seen:





FLORIDA GEOLOGICAL SURVEY


Loc. J-3. A road cut on highway Fla. 73 in the SE 1/ SW 1/4
sec. 30, T. 5 N., R. 10 W., exposes three feet of brownish-gray,
clayey Suwannee limestone with molds of Lepidocyclina sp. and
Pecten sp. below two feet of gray limestone. The elevation of the
top of the limestone is 143 feet.

Suwannee limestone is exposed southward along the Chipola
River between localities J-25 and J-57 from the SW 1/4 sec. 14, T.
4 N., R. 10 W. to the south side of sec. 6, T. 2 N., R. 9 W. A sink-
hole to an underground stream (loc. J-32) on the east bank of the
Chipola River in the south side SW 1/4 NW 1/4 sec. 12, T. 3 N., R.
10 W. contained well preserved echinoids, identified by C. Wythe
Cooke as probably Clypeaster oxybaphon Jackson. Kuphus in-
crassatus was observed in the SE 1/4 NW 1/4 sec. 19, T. 3 N., R. 9
W. (loc. J-46) on the east bank of the river in a hard, crystalline
limestone that extended about five feet above the water. The Su-
wannee limestone beds have a dip of 64 feet per mile (loc. J-51) just
north of the Sink Creek bridge across the Chipola River in the
NE 1/4 SE 1/4 sec. 30, T. 3 N., R. 9 W. (figure 14). Kuphus incrassa-
tus was found in a porous, hardened limestone which extended four
and one-half feet above the water level near the center of the NE
1/4 sec. 31, T. 3 N., R. 9 W. (loc. J-53). Kuphus incrassatus and
Lepidocyclina sp. are to be found on the west bank of the river,
center north side NE 14 NE 14 sec. 6, T. 2 N., R. 9 W., (loc. J-54),
in a tan weathered limestone with drusy cavities and calcite-filled
veins. At a very wide shoal in the river (loc. J-57) at the center of
the south side of the SW 1/ SE 1/4. sec. 6, T. 2 N., R. 9 W. hard, dense
to porous, tan limestone containing Kuphus incrassatus and other
mollusks is exposed. Unquestioned Tampa limestone was found 1/8
of a mile downstream from this point.
Just north of Marianna, along a graded road that joins Fla.
Highway 167 just west of the Chipola River (loc. J-98, J-99, J-102),
greenish bentonitic clays overlie the lowermost bed of the Suwannee
limestone in the road bed. J-98 is located in the NW corner sec. 34,
T. 5 N., R. 10 W.; J-99, at the entrance to an abandoned CCC camp,
SE corner NW 14 NW 1/4 sec. 34, T. 5 N., R. 10 W.; and J-102 SW
1/4 SE 1/ sec. 28, T. 5 N., R. 10 W.
Loc. J-177. A sinkhole in the NE 1/4 SW 1/4 sec. 12, T. 4 N., R.
9 W., just north of the highway (Blue Springs detour) exposes
about 25 feet of Suwannee limestone which is covered by terrace
sands and gravel. The elevation of the land surface around the
sink is 122 feet. Just east of the limestone sink there is a 20 foot





GEOLOGY OF JACKSON COUNTY, FLORIDA


sinkhole in which only terrace sands and gravels were observed
when it was visited in 1948.
Loc. J-166. Residual boulders of Suwannee limestone are found
in the woods east of the road in the northwest corner of the NE 1/4
sec. 3, T. 6 N., R. 8 W. The elevation of the land surface is 121 feet.
Loc. J-175. At a roadside exposure, NE 1/4 NE 1/4 sec. 29, T. 5
N., R. 11 W. about 5 feet of Suwannee limestone, similar to that
at J-13, is weathering to a greenish-brown sticky clay. The elevation
at the top of the Suwannee limestone is 163 feet. Overlying this
limestone and extending to the top of the hill (elevation 185 feet)
are greenish white clays that appear to be the same as those clays
assigned to the Tampa formation in the southern part of the
county. This is the best exposure in central Jackson County of
the clays that overlie the Suwannee limestone.
Loc. J-182. A residual boulder or a pinnacle of Suwannee lime-
stone in which Lepidocyclina sp. was observed is exposed on the
north side of the hill in a roadside ditch near the NW corner NE 1/4
NE 14 sec. 7, T. 4 N., R. 11 W. The elevation of this locality is
estimated to be not greater than 150 feet and this appears to be
the top of the Suwannee limestone in western Jackson County.
Neither residual boulders nor bedrock outcrops that could be re-
ferred to the Suwannee limestone were found in southwestern
Jackson County at elevations above the contact as shown in the
structure section, Plate V.
Loc. J-171. A sinkhole in the woods west of the road in the NW
1/ SW 1/ sec. 28, T. 4 N., R. 11 W. exposes about 5 feet of tan
Suwannee limestone overlain by sandy clays and clay. The eleva-
tion of the top of the limestone is 106 feet. This is one of the best
exposures of the Suwannee limestone in the southwest part of the
county. The clays overlying the Suwannee limestone are believed
to belong to the Tampa formation.
Loc. J-165. At a roadside outcrop, located near the center of the
N 1/2 NW 1/4 sec. 22, T. 4 N., R. 11 W. at the east side of Rhabb's
Valley on Fla. Highway 276, there is exposed, at an elevation of
93 feet, a small patch of tan, clayey marl, overlying chalky white
Marianna limestone, which appears to be lowermost Suwannee.
The clayey marl, of Suwannee age, is similar to that exposed in
the upper bed at loc. J-13.
Loc. J-192. A sinkhole in the woods south of Fla. Highway 276
in the NW 14 SE 1/ sec. 13, T. 4 N., R. 11 W. exposes about 20




FLORIDA GEOLOGICAL SURVEY


feet of tan, clayey, dolomitic limestone. The elevation of the top
of this Suwannee limestone section is 110 feet.
The Suwannee limestone was encountered in the following wells:
W-l, W-4, W-7, W-547, W-276, W-1356, W-1357, W-1358, W-1359,
W-1362, W-1364, W-1478, W-1479, W-1783, W-1793, W-1794,
W-1824, W-1873, W-1987, W-2194, W-2251, W-2260, W-2328,
W-2329, and W-2409. Appendix I gives the depth at which the
formation was encountered.

MIOCENE SERIES
TAMPA FORMATION
Historical.-For a historical summary of the Tampa formation
the reader is directed to Florida Geological Survey Bulletins 21
and 29. Since this formation is primarily clay and clayey marls
in Jackson County, the term Tampa formation will be used in this
report, but stratigraphically the unit is the same as the Tampa
limestone defined by Cooke and Mansfield (1936, p. 71). In the
southwestern part of Jackson County, beds that may belong to
younger formations have been included in the Tampa formation
but these beds lie at elevations that are higher than those expected
for the Tampa formation. No fossils were found in these beds, and
lithologically they are similar to the Tampa formation.

Definition.-The Tampa formation of this report consists of
white, gray, and green clays that are frequently calcareous, and, in
the southeastern part of the county, white, arenaceous and argil-
laceous limestone. The Tampa formation is overlain by the clayey
sands and gravels of the terrace deposits and underlain by the
buff to tan limestones and dolomitic limestones of the Suwannee
limestone.

Lithology.-The Tampa formation is more calcareous in the
southeastern part of the county and along the Chipola River, and
it is more argillaceous in the western and northwestern parts of
the county. The whole formation is characterized by the presence
of fine, scattered quartz grains. The gray and white clays and argil-
laceous limestones commonly have, in addition to the fine sand,
scattered pellets of green clay similar to that which occurs in the
beds within the formation as exposed above Jim Woodruff Dam
near Chattahoochee.

Thickness and Structure.-The Tampa formation at the Jim
Woodruff Dam is 170 feet thick; at Sink Creek it is no more than





GEOLOGY OF JACKSON COUNTY, FLORIDA


100 feet thick; and in the southwestern part of the county near
Round Lake it is about 70 feet thick (figure 16). Figure 17 shows
the configuration of the top of the Tampa formation as reconstruc-
ted from wells and outcrops.

Paleontology.-With the exception of a few calcareous zones,
the Tampa formation as exposed in Jackson County is not very fos-
siliferous. No fossils were found in any of the clays although at
some localities small fossiliferous boulders of silicified clay, or clay
in which secondary calcification had occurred, were found. These
fossils, or their prints, are poorly preserved.
Reference should be made to Mansfield's report (1937, pp. 31-33)
for lists of fossils from four fossiliferous zones in a section exposed
along the road at the east end of Victory Bridge on Highway U. S.
90 in Gadsden County.

Local Details.-The Tampa formation crops out in the southern
part of Jackson County (Plate I) and thick sections occur in both
the southeastern and the southwestern portions of the county. Be-
cause it is predominately clay, the parts of the county underlain by
the Tampa formation have more relief than the areas of the county
underlain by purer limestone. These clays are quite blocky and
tough and are effectively eroded only by stream abrasion.
The course of Dry Creek is controlled by the southward dip of
the Tampa beds and of the underlying Suwannee limestone. The
escarpment south of Dry Creek is a result of the lateral erosion by
this subsequent stream over a long period of time (Plate II). Simi-
larly, both the Flint River and the Apalachicola River are bordered
to the southeast in this general area by a high escarpment that
has resulted from the lateral erosion of these streams down the
regional dip.
The following significant localities show typical expressions of
the Tampa formation in Jackson County:
The most complete Miocene section exposed in the Jackson
County area is to be found along the access road at the east end of
the Jim Woodruff dam, in Georgia, on the Apalachicola River. The
top of the Tampa formation at this locality has an elevation of
169 feet. Mansfield (1937, p. 32) gives an elevation of 165 feet for
station 13854, bed 12 (W. C. Mansfield and F. S. MacNeil), of the
section exposed about one mile south of the Jim Woodruff Dam
along the road at the east end of Victory Bridge in Gadsden County.












PROBABLE THICKNESS
OF THE
TAMPA FORMATION
--0- THICKNESS IN FEET
iJmUL LIMIT OF WOTROP
o WELL SAMPLE
X SURFACE OUTCROP
PROBABLE PRE TAMPA POST SUWANNEE FAULT

SCALE
4 0 4 8 IlMIt


tR I W | R JI w R w pr II 0 I 2 A n I R f W m i

Figure 16.-Map, probable thickness Tampa formation.


0 5 IAL 4 W I ft 3










STRUCTURE MAP
JACKSON OF THE
OF THE
STAMPA FORMATION
S-Conrour datum mean sea lrvel
T '.--50- CONTOWR

0 WELL SAMPLE
-- -4 8 SURFACE OUTCROP
S. __ PROBABLE PRE TAMPA POST SUWANNEE FAULT
W '2252 SCALE
I W- . /W1364 4 06



S251









T i~. i ~ ------ ----- ----- --- ^I ^ r
2z







WASHINGTON o-" "- --.



SBAY CALHOUN
LIBERTY
C




S I R 13 2 2 R I I W I 9 w I I 4 A e W

Figure 17.-Structure map of Tampa formation.




FLORIDA GEOLOGICAL SURVEY


Figure 18 shows the upper part of the section at the east end of
the Jim Woodruff Dam, and figure 19 is a composite section of the
Tampa formation at the east end of the dam. This section was
partially measured when, unfortunately, the excavation in the
floodplain of the river was filled before precise levels and collections
could be made. The elevations from 122 feet to the top of the Tampa
formation section, however, were surveyed with a level and rep-
resent true elevations above sea level. The elevation of 40 feet
shown in figure 19 is also a true elevation obtained from the U. S.
Engineers at the dam, and represents the elevation of one of their
stations in bedrock at the bottom of the foundation cut in the flood-
plain. Several "cuts" of cores from U. S. Engineer core holes at
the dam are on file with the Florida Geological Survey, and eleva-
tions for these core holes are available there.
The white argillaceous limestone exposed in both the Jim Wood-
ruff Dam section and the Old Chattahoochee Landing section at
the east end of Victory Bridge contains fine, scattered quartz sand.
The section at the dam exposes four beds of green clay along the
access road. The lowest of these clays appears to have been de-
posited over the mudcracked surface of the underlying argillaceous
limestone (elevation 135 feet). Two additional green clays were





















Figure 18.-Upper part of Tampa formation as exposed at east end of
Jim Woodruff Dam on Appalachicola River, just north of Chattahoochee, in
Decatur County, Georgia.





GEOLOGY OF JACKSON COUNTY, FLORIDA


exposed in the dam foundation excavation below elevation 122 feet
and above elevation 40 feet in about the position shown in figure 19.


Elev.
169'- Unconformity
Grey to brown sandy is., thin cprbonnceous clays at top.
Massive chalky Is., thin bedded at top with some green
clay seams and lenses.
150' White ls., fossiliferous lenses, green and clayey at top.
146' Soft clay, lower part fossiliferous.
19, Thin green bed at base, white marl at ton.
139'- Chalky, sandy, vesicular la.
135' Green clay with fish bones and manatee rib at base.

White, fossiliferous, chalky limestone, upper surface
122' I mud cracked.

Light grey to white clayey, finely sandy marl.


Olive green plastic clay.


Soft, tan to white clayey marl.



-Fossiliferous zone.

S 2 foot bed of green clay


I I Fossiliferous zone.


40'- Base of Trench


I Kuphus incrassatus, top of Suwannee Is?



Figure 19.-Composite section of the Tampa formation at east end of Jim
Woodruff Dam. Elevations at 0 feet, 40 feet, and above 122 feet are accurate.
Elevations shown to the left were determined by levelling.




FLORIDA GEOLOGICAL SURVEY


Loc. J-137. An outcrop at the Tee road intersection in the center
of the NW 1/ sec. 20, T. 4 N., R. 7 W. exposes about 10 feet of white,
siliceous clay. The elevation at the top of these siliceous boulders
is 175 feet.

Loc. J-66. A roadcut near NW corner SE 1/ NW 1/ sec. 30, T.
4 N., R. 7 W. exposes 63 feet of tough stickey, gray clay and marl
that extends almost to the top of a hill which has an elevation of
238 feet. At this locality the clay tends to weather to cherty nodules
and at locality J-67, the crossroads at the center of the north side
NW 1/4 sec. 31, T. 4 N., R. 7 W., at an elevation of 197 feet, a similar
deposit was found.

Loc. J-65, a small waterfall, on a creek near a flooded sinkhole
(Falling Branch Sink) is situated near the center of sec. 30, T.
4 N., R. 7 W. and exposes a tan to white sandy limestone.

Loc. J-112, a roadside outcrop, just north of the railroad crossing
at the approximate center of sec. 36, T. 4 N., R. 7 W. exposes about
5 feet of white fossiliferous Tampa limestone. The elevation at the
top of the limestone is 135 feet.

Loc. J-64, a roadside outcrop, located 2.8 miles south of Sneads
near the center of sec. 9, T. 3 N., R. 7 W. exposes about 5 feet of
pinnacled, sandy, chalky, white Tampa limestone which is overlain
by terrace deposits. The elevation of the top of the limestone at
this exposure is 140 feet.

Loc. J-69, a creek bank, east of the road in the SE 1/ NW 1/
sec. 16, T. 3 N., R. 7 W. exposes 9 feet of greenish clay that grades
upward into a creamy, white marl. The elevation at the top of
the marl is 143 feet.
Loc. J-70, a creek bank, on the east side of the road, NW 1/4
SW 1/4 sec. 16, T. 3 N., R. 7 W. exposes 10 feet of white argillaceous
limestone overlain by a greenish clay. The elevation at the top of
the green clay is 131 feet.
Loc. J-71, a roadside ditch, at about the center of NW 1/4 sec.
21, T. 3 N., R. 7 W. exposes a similar white, clayey, sandy lime-
stone. The elevation of the road at this locality is 133 feet.
Loc. J-111, an outcrop at the south end of Ocheesee Pond at
about the center of the S 1/2 sec. 18, T. 3 N., R. 7 W., exposes 5 feet
of soft, white, sandy marl. The elevation at the top of the marl
is 134 feet.




GEOLOGY OF JACKSON COUNTY, FLORIDA


Loc. J-133, a road cut in Calhoun County, NW 1/4 NE 1/4 sec. 6,
T. 2 N., R. 7 W., exposes white, soft chalky Tampa formation over-
lain by about 5 feet of green clay. The elevation at the top of the
white limestone is 97 feet. The white limestone and green clays
are overlain by terrace sands and gravel.
Loc. J-187, a roadside exposure at the top of a hill on the graded
road near the center of the south section line sec. 18, T. 4 N., R.
8 W., exposes Tampa type clay. The elevation of the road at the
top of the hill is about 150 feet. A series of ponds just west of the
road along a line trending northeast probably marks the Oligocene-
Miocene contact.
Loc. J-140, a sinkhole in the woods at the approximate center of
sec. 21, T. 4 N., R. 8 W., exposes 5 or 6 feet of white, clayey limestone
with greenish clay-ball inclusions which are similar to those at
the Jim Woodruff Dam section near Chattahoochee. The elevation
of the top of the limestone at this sinkhole is 157 feet.
Loc. J-82, a limestone pinnacle at the north edge of the highway
(Blue Springs detour) in the SW 1/4 NE 1/4 sec. 21, T. 4 N., R. 8 W.,
exposes white, hard Tampa limestone overlain by greenish clay. The
elevation at the top of the limestone is 108 feet.
Loc. J-114, the side of a hill around a sink near Shady Grove, at
the approximate center sec. 14, T. 3 N., R. 8 W., exposes small
patches of tan, clayey Tampa limestone and gray clay.
Loc. J-115, a sinkhole at the site of an old grist mill in the NW
1/4 NW 1/ sec. 25, T. 3 N., R. 8 W., exposes 12 feet of Tampa lime-
stone. The elevation at the top of the limestone is 144 feet. This
is a good exposure and the softer, white limestone is rather fossili-
ferous. No road extends to this locality and it is best to inquire for
local directions to the site of the old grist mill.
Loc. J-129, a wagon road and sink hole in the approximate center
of the N 1/2 sec. 27, T. 3 N., R. 8 W. exposes about 14 feet of marl
of the Tampa formation. The elevation of the top of the marl is
136 feet.
Loc. J-131, the creek bed under a bridge in the NW corner NE 1/4
sec. 32, T. 3 N., R. 8 W., exposes an unfossiliferous, white to cream
colored, clayey limestone.
Loc. J-119, a roadside outcrop in Calhoun County in NE 1/4
NW 1/ sec. 11, T. 2 N., R. 8 W., exposes 10 feet of very clayey, white
marl. The elevation at the top of this marl, which is overlain by




FLORIDA GEOLOGICAL SURVEY


terrace deposit, is 120 feet. The marl weathers to a greenish-brown
clay which cracks and crumbles when dry. This is considered to
represent the upper part of the Tampa formation.
Loc. J-132, a road cut in Calhoun County, just south of the
bridge near the center of the west side sec. 3, T. 2 N., R. 8 W., ex-
poses approximately 8 feet of soft, clayey, sandy limestone overlain
by 2 feet of green, plastic clay. The elevation at the top of the
white limestone is 114 feet. This is considered to be uppermost
Tampa formation. Overlying the green clay of the Tampa forma-
tion are crossbedded sands and gravels of a terrace deposit.
Loc. J-141, a steephead near Alliance, near the center of the S
1/2 NE 1/4 sec. 34, T. 3 N., R. 9 W. just west of the church, exposes
8 feet of gray, sandy clay below about 15 feet of crossbedded sands
and gravel of a terrace deposit. The elevation of the top of this
sandy clay is 180 feet. This steephead is of particular interest since
a spring emerges at the contact between the clay of the Tampa
formation and the overlying sands and gravels. The stream channel
has been cut out of the overlying coarser deposit. This steephead is
developing headward and it has recently cut back across the road
(figure 3).
Loc. J-58, at a boat landing on the west bank of the Chipola
River near the center of the W 1/2 NE 14 sec. 7, T. 2 N., R. 9 W., soft,
white, sandy Tampa limestone is exposed. This limestone crops
out along the river to the south into Calhoun County. The lime-
stone is characterized by fine, scattered quartz grains and varies
from white to light brown in color.
Loc. J-195, a roadside outcrop at the north side of Fla. Highway
276 in the center of the NE 1/, sec. 8, T. 4 N., R. 10 W. exposes 10
feet of very plastic, gray to white, clay at an elevation of 130 feet. A
similar clay that weathers to white chert nodules, typical of clays of
the Tampa, can be seen at the southwest corner of the road inter-
section at SE 1/4 NE 1/4 sec. 13, T. 4 N., R. 11 W. at an elevation of
135 feet. These clays are similar in color, texture, and composition
to the clays of the Tampa formation in the southern part of the
county, and they are here correlated with the Tampa formation. The
clay at J-195 is overlain by bog-iron and terrace deposits ( figure
20).
Loc. J-181, a roadside outcrop on the S side SE 14 SE 14 sec.
15, T. 3 N., R. 10 W., exposes 33 feet of plastic, greenish-gray clay
of the Tampa formation. The elevation at the top of this rather
pure plastic clay is 156 feet.




GEOLOGY OF JACKSON COUNTY, FLORIDA 67


Figure 20.-Locality J-195. Tampa formation clays overlain by "bog iron"
and terrace deposits on highway Fla. 276 east of the Florida Industrial School
for Boys.

Loc. J-159, a cut at a road corner at the SE corner sec. 16, T.
3 N., R. 10 W. exposes approximately 15 feet of rather pure, gray,
plastic, blocky clay. The elevation of the road corner is 147 feet.
This clay is placed in the Tampa formation.

Loc. J-155, a sinkhole just south of W. B. Pumphrey's house
in the center W 1/2 SW 1/ sec. 17, T. 3 N., R. 10 W. exposes 5 feet
of greenish-gray, clayey limestone. The elevation of the top of this
limestone is 144 feet.

Loc. J-90, a sinkhole in the SE 1/ SE 1/ sec. 18, T. 3 N., R. 10
W. exposes 10 feet of sandy, white, glauconitic, argillaceous lime-
stone. The sink is west of the road a short distance.

Loc. J-101, a steephead located near center of the SE 14 sec.
20, T. 3 N., R. 10 W. on the east side of the road exposes what is
probably the uppermost clay of the Tampa formation overlain by
about 30 feet of terrace sands.

Loc. J-95, a roadside outcrop in the center of the W side NE 1/
sec. 22, T. 3 N., R. 10 W. exposes about 10 feet of gray-white marl.
The elevation at the top of this marl is 139 feet.




FLORIDA GEOLOGICAL SURVEY


Loc. J-96. Residual boulders at the top of the hill in the woods
west of highway Fla. 73 in the center of N 1/2 SE 1/4 sec. 23, T. 3 N.,
R. 10 W. range from dense and crystalline to soft, porous, white,
sandy limestone. The elevation at the top of the hill is 132 feet.
While badly weathered, these boulders are very fossiliferous.
Loc. J-153, a steephead east of the road at the center of the W
side NE 1/ sec. 27, T. 3 N., R. 10 W., exposes, at an elevation of 225
feet, about 3 feet of tan, sandy clay of the Tampa formation which
is overlain by 50 feet of terrace sands. This is almost certainly
near the top of the Miocene section in Jackson County and this
clay is referred to the Tampa formation, but it is possible that a
portion of it is Alum Bluff in age.
Loc. J-176, a roadside outcrop near the SE corner NW 1/4 sec.
28, T. 5 N., R. 11 W. exposes about 8 to 10 feet of white, blocky,
sandy clay and clay. The elevation of the top of the clay is 155
feet. This locality is referred to the Tampa formation because the
clays are similar to clays in the southern part of the county that
were referred to the Tampa formation. A similar white clay over-
lies the Suwannee limestone at locality J-175 farther west on this
same road.
Loc. J-93. Residual boulders of the Tampa formation occur along
the road and extend to the top of the hill south of the road NW 1/
SE 1/ sec. 7, T. 3 N., R. 11 W. The elevation of the road where
this float is first observed is 143 feet. The elevation at the top of
the hill south of the road is about 175 feet. The top of this hill
appears to have been leveled by terrace development.
Loc. J-92. At the bottom of a sink hole in the SW 1/ NW 1/
sec. 13, T. 3 N., R. 11W., a small patch of soft, white, argillaceous
Tampa limestone is exposed. This sink is about 100 yards north
of the road and the land surface has an approximate elevation of
110 feet.
Loc. J-160, a road cut at the NW corner SW 1/4 sec. 14, T. 3 N.,
R. 11 W., exposes fossiliferous boulders or pinnacles of tan to white
clayey marl. The elevation of the road corner is 150 feet. The
marl is overlain by terrace gravels and sands in which the bedding
is confused by slump. This outcrop may consist only of residual
boulders which represent higher beds. The fossils are poorly pre-
served as external molds.
Loc. J-163, a sinkhole in about the NW 1/4 NW 14 sec. 16, T. 3 N.,
R. 11 W., exposes silicified fossiliferous boulders of the Tampa




GEOLOGY OF JACKSON COUNTY, FLORIDA


formation in rather pure, plastic clay. The elevation of the highest
silicified limestone boulder is 171 feet. Only boulders could be found
in the soil around this sink and it is probable that they represent
silicified zones in the clayey limestone. Augerholes at this locality,
located to one side of the sink and carried below the level of the
boulders, failed to encounter a rock zone, but the clay analysis of
the augerhole samples (Appendix II, loc. J-163) indicated a limey
zone at a depth of 6-7 feet.
Loc. J-188. Boulders of limestone in the field near the center of
the west line NW 1/ sec. 18, T. 3 N., R. 11 W. show occasional faint
mollusk imprints. The elevation of this field is 177 feet.
Loc. J-164. A field outcrop underneath the REA power line on
the A. C. Siefert farm at the SW corner NW 1/4 sec. 35, T. 4 N., R.
12 W. exposes very hard recrystallized limestone at an elevation of
171 feet. Archaias? sp. was noted in this rock and it is referred
to the Tampa formation.
Loc. J-87, a railroad cut at the north edge of Round Lake in the
NE 1/ SW 1/4 sec. 13, T. 3 N., R. 12 W., exposes a clay section which
is assigned to the Tampa formation. The elevation at the top of
this section, 265 feet, seems to be too high for the Tampa formation
when compared with that of other exposures, and this clay section
may represent the Alum Bluff group, or possibly younger Miocene
formations. These unfossiliferous clay beds have been folded,
probably because of subsidence, the result of solution of the under-
lying limestone (figure 21).
The Tampa formation was encountered in the following wells:
W-l, W-4, W-7, W-547, W-276, W-1478, W-1788, W-1796, W-1813,
W-1824, W-1834?, W-1872, W-1874, W-2194, W-2251?, W-2260,
W-2409, W-2433, and W-2531. Appendix I gives the depth at which
the formation was encountered.

POST-MIOCENE DEPOSITS

Historical.-The complicated history of the terminology ap-
plied to the post-Miocene deposits of Florida is adequately reported
in Florida Geological Survey Bulletins 21 and 29 and need not be
repeated here.

General Discussion.-Vernon (1951) suggests that the deposits
underlying each terrace surface be given a formational name the
same as that of the associated terrace. Because of the difficulty of




FLORIDA GEOLOGICAL SURVEY


Figure 21.-Locality J-87. Railroad cut at Round Lake showing Miocene?
clays (Alum Bluff?) overlain by terrace deposits.

dating these deposits in any other way, this seems to be the most
satisfactory system. The terrace deposits underlying the terrace
surfaces are therefore named as follows:

Terrace Surface underlain by Terrace Deposit
Pamlico Pamlico fm.
Wicomico Wicomico fm.
Okefenokee Okefenokee fm.
Coharie Coharie fm.
Cooke (1945) referred the deposits underlying what is here
called the Delta Plain Highlands to the Citronelle formation of Plio-
cene age. Because it is not feasible to rule out an early Pleistocene
age for at least a part of these deposits, no definite age is assigned
to these deposits and they are merely considered to be Pliocene? or
Pleistocene in age (Vernon, 1942, p. 134; 1951, p. 15).
It seems agreed that the highest of these post-Miocene terrace
deposits are the oldest and that the lowest are youngest. Further, in
recent years it seems to be agreed that some, if not all, of the ter-
races lying below the Delta Plain Highland surface are related to
sea level fluctuations of the Pleistocene.
Plate II shows the extent of the various terrace surfaces and
post-Miocene deposits as they occur in Jackson County. The sur-





GEOLOGY OF JACKSON COUNTY, FLORIDA


faces are made irregular by dissection, and when topographic maps
become available for the area, it will be possible to add considerable
detail to the map.

Lithology and Thickness.-The terrace deposits consist of clayey
sands, sands, and gravels that change laterally and vertically within
short distances. Most deposits are cross-bedded. Locally, "limonite"
cements the sands and gravels into a hard, dense, ferruginous sand-
stone.
The stream terrace deposits range in thickness from 30 to 50
feet, but the thickness of deposits of the so-called Citronelle forma-
tion is unknown. It is estimated to be approximately 80 feet thick
in southwestern Jackson County.

Residual Boulders.-The stream terrace deposits have fre-
quently incorporated residual boulders of formations that are strati-
graphically higher than those now cropping out at the surface. The
Suwannee limestone in particular has contributed such boulders to
the terrace deposits. A drainage canal that crosses highway Fla.
71, 1.1 miles south of Malone, exposes these boulders incorporated
in the sands and gravels of the Pamlico formation (figures 22 and
23). Vernon (1942, pp. 130-131) described how these boulders
may be let down by erosion and undercutting during periods of
valley cutting so that they slumped down valley walls and thus be-
came incorporated in the terrace deposits. Cooke (1923, p. 4)
considered many of these larger boulders to be in place and mapped
them as Glendon limestone, and he later (Cooke, 1935, pp. 1170-
1171) applied the name Flint River formation to deposits in Georgia
which he considered to extend into Jackson County (Cooke, 1945,
Plate 1). MacNeil (1946) shows how these residual boulders are
incorporated into the terrace, which he shows on the map as resi-
duum.

SEDIMENTATION, BIOFACIES, AND STRUCTURE

The distribution of two distinct biofacies of Jackson Eocene
age is related to the present structure of the Jackson County area.
These two biofacies are interpreted as indications that the present
structural pattern in Jackson County was in existence, or was de-
veloping, as early as Jackson time. The absence of the upper Clai-
borne and the Moodys Branch formations in Jackson County appear
to indicate that the structural pattern was established at least as
early as the beginning of Jackson time.





72 FLORIDA GEOLOGICAL SURVEY


.. -. :.Ih .


Figure 22.-Drainage canal south of Malone cut in terrace deposits.
Looking west from highway Fla. 71.


Figure 23.-Residual boulders of Suwannee limestone in terrace deposits
forming the sides of the drainage canal south of Malone.





GEOLOGY OF JACKSON COUNTY, FLORIDA


Biofacies Evidence.-Lowman (1949, pp. 1950-1964), in a dis-
cussion of the distribution of Foraminifera in Recent sediments of
the Gulf of Mexico, reported that the family Buliminidae, especially
the genera Uvigerina and Bolivina, were dominant in waters of the
inner bathyal zone and that conspicuous numbers and varieties of
the Lagenidae were characteristic of the outer neritic zone. He
placed the boundary between the neritic and bathyal zones at a
water depth of 600 feet.

During the study of the Ocala group in Jackson County, only
the fauna characterized by the genera Asterocyclina, Lepidocyclina,
Operculina, and Operculinoides was encountered until the samples
from well W-1987 were examined. The strata in this well, although
containing a few specimens of Asterocyclina and Lepidocyclina,
were characterized by many specimens of Uvigerina, Bolivina, Rob-
ulus, Marginulina, and Nodosaria. The abundance of species of small
Foraminifera, the rarity of the orbitoidal and camerinid Foramini-
fera, and the generic composition of the fauna is unlike that which
occurs in most exposures of beds of the Jackson stage throughout
Florida. A similar Ocala group fauna that contained no large Fora-
minifera was described by Cole (1944) from cuttings of the city
of Quincy, Gadsden County, water well, W-4. Published faunal lists
for Ocala group localities near Whatley and Grove Hill, Clarke
County, Alabama (Cushman, 1935, localities 1/38 and 7159, p. 4)
contain a fauna characterized by Uvigerina spp., Bolivina spp., and
several genera and species from the family Lagenidae.
Faunas characterized by the Buliminidae and the Lagenidae
occur in scattered areas and are not distributed generally. Further,
this fauna is found only in districts which appear to be structurally
"low." In Jackson County the fauna characterized by Lepidocyclina,
Asterocyclina, Operculina, and Operculinoides occurs only in areas
which are structurally high.

Because the distribution of these two different faunas in the
Jackson County area appears to be related to the structure, the
possibility exists that the structural highs and lows were in exis-
tence, or were developing, when the Ocala group of limestones was
being deposited, and that the distribution of these faunas was con-
trolled by the depths of the water.

Lowman (1949) Phleger (1951), and others have published
studies of foraminiferal distribution in Recent sediments from the
Gulf of Mexico. Lowman (1949), Bandy (1953) and others have




FLORIDA GEOLOGICAL SURVEY


graphically shown for each genus or species its percentage of the
total population at various depths. A comparison between Eocene
species and Recent species, with regard to depth ranges, is not pos-
sible, of course, and a comparison of the relative distribution of
Eocene and Recent genera might be open to serious question. The
following comparisons between Eocene and Recent foraminiferal
distribution are made at the family taxonomic level because it is
believed that the minimum changes in environmental habit and in
relative abundance are to be expected at this taxinomic level.
Further research in the ecology of the Foraminifera may indicate
that comparisons may be made over the Eocene-Recent time span
between more refined taxonomic groups. For the purposes of this
report, comparisons at the family level are adequate to define the
significance of the two biofacies.
Two samples from the uppermost part of the Ocala group in
Jackson County were selected for a comparison of their foramini-
feral content. The shallower water biofacies of the Crystal River
formation is represented by a sample from the Bumpnose member
of the Crystal River formation at locality J-5. The deeper water bio-
facies of the Gadsden limestone is represented by the sample from
288-298 feet of well W-1987. These two samples are from the same
stratigraphic horizon. The percentages shown in figure 24 are
based upon 236 specimens picked from well W-1987, depth 288-298,
and 328 specimens from locality J-5. Specimens of the "large"
Foraminifera were not picked for this comparison but they are rare
in well W-1987 and abundant at locality J-5, where they often con-
stitute over 90 percent of the total volume of the rock.
The Lagenidae constituted 22.45 percent and the Buliminidae
constituted 27.45 percent of the total specimens in the sample from
well W-1987. By contrast, the Lagenidae constituted only 18.2
percent and the Buliminidae constituted only 10.1 percent of the
specimens from locality J-5., which is structurally higher than well
W-1987. Samples from the City of Quincy well W-4 were not
counted for percentages, but the fauna is similar to that of well
W-1987 except that there are no "large" Foraminifera in well W-4.
The "large" Foraminifera are always more abundant in the samples
with lower percentages of the Lagenidae and Buliminidae, and as
the latter increase in percentage of the total fauna, the "large"
Foraminifera become more scarce. The Lagenidae and Buliminidae
become more frequent downdip to the southeast, and beyond the
Cypress fault they become the dominant elements of the fauna.
Southeast of the Cypress fault the Lagenidae and Buliminidae






Well W-1987 (288-298') upper Gadsden limestone
Family
Polymorphinidoe
Planorbulinidoe
Textuloridoe
Vern eui/nidoe
Valvulinidae
Globigerinidae N
Ro to liidoe
Lagenidoe
Anomaloni/doe
Buliminidoe
Misc.


40%


30%


2


10%


Locality J-5, Bumpnose member
Family
Polymorphinidae
222a Plonorbuini/doe
Textuloridoe
A Ve rneuilinidoe
S/ Vo/vulinidoe
7 Globigerinidoe
//1 Roto//idae
/////////////////// Lagenidoe
2 Anoma/inidoe
/II Buliminidoe
/ //7Misc.
Mostly poorly preserved Anomalinidae or Rotaliidae
10% 20% 30% 40%


Figure .A comparison of the
the upper Gadsden


Foraminiferal Faunas of the Bumpnose limestone member and
limestone. "Large" Forominifera omitted.


I m I I


3





FLORIDA GEOLOGICAL SURVEY


dominate the fauna to lower and lower stratigraphic levels until
at Quincy the entire Jackson Eocene section is dominated by them
and there are no specimens of Lepidocyclina, Asterocyclina, and
Operculinoides to be found.
The Jackson stage foraminiferal fauna of well W-1987 is in-
terpreted as an outer neritic or inner bathyal fauna as these zones
were defined by Lowman (1949, pp. 1950-1964). A comparison of
the data discussed above with Phleger's foraminiferal distribution
charts (Phleger, 1951, tables 10-30) suggests that the sample from
locality J-5 would indicate a water depth of roughly 150-160 feet
at the time of deposition. The same comparison suggests that the
depth of the water at the time of deposition for the sample from
well W-1987 was about 250-260 feet. These are interpreted as mini-
mum depths. The sample from well W-1987 is structurally 331 feet
lower than locality J-5 at the present time. At least 150 feet of the
present structural interval between the two localities can be re-
moved, because of post-Jackson structural movements, mainly the
displacement caused by the Cypress fault, so that a depositional
difference in depth of 181 feet, as a maximum, existed when the
sediments were deposited.
It should be understood that no specific depths in feet are being
formally proposed for the Eocene faunas discussed above, but it
seems that the depth zones mentioned above are reasonable. It is
my opinion that the faunas dominated by the Lagenidae and the
Buliminidae are deeper water faunas than those in which the
Orbitoididae and Camerinidae dominate and in which the Bulimin-
idae in particular are not dominant. Exact depth correlations be-
tween Eocene and Recent faunas cannot be made because different
species are involved. Similarly, exact depth comparisons cannot be
made between Eocene and Recent faunas based upon their generic
frequencies with certainty because of moderate shifts in the generic
frequency composition of faunas during that time interval. It is
probable, however, that relative abundance of most families is
much the same for a given environment today as it was in the
Eocene. Certainly, families should change their overall environ-
ment requirements slower than lower taxonomic units.

The important point is that the water was appreciably deeper
southeast of the Cypress fault than to the northwest during latest
Jackson times. This indicates that the present regional structural
pattern was established as early as Jackson time. The absence of
the upper part of the Claiborne Eocene and the lower Jackson





GEOLOGY OF JACKSON COUNTY, FLORIDA


Eocene in the Jackson County area is more plausible when it is
understood that the present structural pattern was in existence
then. Therefore, it is not too surprising that movement along the
Cypress fault occurred along a zone of flexure after the deposition
of the Suwannee limestone of late Oligocene age, and before, or
during, the first phases of deposition of the Tampa formation of
early Miocene age. All of this indicates structural continuity, re-
flected in both the sediments and the faunas, that began at least as
early as the Jacksonian and which has not been destroyed or ap-
preciably modified. Exactly how early this structural pattern origi-
nated is not known. More deep wells between Jackson County and
Tallahassee must be drilled before sufficient data will be available
to determine when this structural pattern originated. Plate IV
shows diagramatically the faunal relationships to the structure in
the area just discussed.

General.-In considering the Tertiary geological history of this
area, the following features are important:
1. A structural high exists in north central Jackson County, in
Holmes County, and northern Washington county (figure 6).
The Oligocene-Miocene contact is an unconformity in the central
part of Jackson County; the contact becomes more nearly conform-
able to the south and southeast (plate III).
2. Deep water foraminiferal faunas are found in structural
lows northwest, northeast, southeast, and south of the structurally
high area.
Deep water upper Jackson foraminiferal faunas are found in
Clarke County, Alabama (Cushman, 1935, facing p. 60, no. 3),
Jenkins County, Georgia (Cushman, 1935, facing p. 60, no. 2),
Gadsden County (Cole, 1944) and southeastern Jackson County in
Florida. These areas are structurally low.
3. The Tertiary sediments thicken toward the southeast and
south away from the structural high (figure 25).
The Suwannee limestone thickens considerably southward from
Jackson County (Plate III).
4. The Bumpnose fauna appears in an area around and to the
north of Marianna and in an area about Tallahassee and probably
extending as far east as Suwannee County. These areas are struc-
turally relatively high and the fauna indicates shallow water (Plate
IV).








ISOPAGHOUS MAP 0
OF THE
UPPER EOCENE, OLIGOCENE
AND
LOWER MIOCENE FORMATIONS
-600- THICKNESS IN FEET DOTTED WHERE UNCERTAIN
-AA"A LIMIT OF OUTCROP
O WELL SAMPLE
X SURFACE OUTCROP
PROBABLE PRE-TAMPA POST SUWANNEE FAULT

SCALE

0 4 I4 t2AMAs





0


U / o

// 0









GADSEN


Figure 25.-Isopach map of the upper Eocene, Oligocene, and lower Miocene formations.





GEOLOGY OF JACKSON COUNTY, FLORIDA


5. Beginning with the Miocene, the sediments in Jackson County
become more elastic to the west and northwest away from the
structural low in Gadsden and Leon Counties.

Crystal River formation.-The uniform thickness of the Crystal
River formation in Washington, Holmes, and Jackson Counties in-
dicates that uniform conditions of deposition prevailed. In wells
W-4 and W-1987, however, the upper part of the Jacksonian section
has fewer large Foraminifera than usual. Small Foraminifera,
however, are abundant in samples from these wells. In well W-1987
the families Buliminidae and Lagenidae are represented by abun-
dant genera, species, and individuals. Regarding the Ocala section
of well W-4, Cole (1944, p. 16) states:

"Various species of Uvigerina of upper Eocene type were found in
virtually every sample and numbers of these occurred in the last sample
(1370 feet). So easily recognized and typical Jackson species as Buli-
mina jacksonensis Cushman and Hemicristellaria fragaria (Giimbel),
variety texasensis (Cushman and Applin) characterize this section to-
gether with Eponides jacksonensis (Cushman and Applin) and Sipho-
nina jacksoncnsis Cushman and Applin."

Cole (1944, p. 16) also mentioned that large Foraminifera are
not present in the portion of W-4 which he assigned to the Ocala
group,, and, although Ocala group large Foraminifera are present
in W-1987, they are relatively rare. Further, neither of these wells
encountered the Lepidocyclina (Nephrolepidina) chaperi zone.
From Lowman's work, (1949, Table II, p. 1956), based on recent
foraminiferal studies in the Gulf of Mexico, the small Foramini-
fera faunas from wells W-4 and W-1987 indicate deep water, pos-
sibly the outer neritic or inner bathyal zone (figure 24).
Cole (1944, pp. 16-17) was concerned about the apparently ab-
normal thickness (690 feet) of the Ocala group in well W-4, and he
suggested that savings may have obscured a lower unfossiliferous
formation. Applin and Applin (1944, fig. 23, pp. 1736, 1737)
assigned the lower part of what Cole considered to be Ocala in
Well W-4 to the Tallahassee limestone.
That the Marianna-Chipley area was a relatively positive seg-
ment during deposition of the Crystal River formation seems to be
borne out by the faunal distribution (Plates III and IV). In struc-
turally high areas, the Ocala group is characterized by abundant
large Foraminifera. In structurally low areas, small Foraminifera
of deep water types are found. It would appear therefore, that






FLORIDA GEOLOGICAL SURVEY


the present general structural configuration was in existence
during the deposition of the Crystal River limestone, and that there
probably was differential downsinking, Holmes, Jackson, and Wash-
ington Counties sinking less than the structurally low areas to the
east and to the south where the Gadsden limestone was deposited.

Bumpnose Member.-It is suggested that the Bumpnose mem-
ber [Lepidocyclina (Nephrolepidina) chaperi zone] represents a
depositional environment located far from land and shallower than
that of the pre-Bumpnose Crystal River. L. (N.) chaperi was not
transported from some other area by currents, because: a) this
species does not occur at any known horizon except the L. (N.)
chaperi zone; b) where it occurs it does so in great numbers;
c) the fauna of the zone is a peculiar one suggestive of a restricted
facies. It is difficult to account for the absence of the L. (N.) chaperi
zone elsewhere on the basis of erosion because it is absent in those
areas where other formations are most complete and where un-
conformities are fewest and of the least magnitude. L. (N.) chaperi
must be confined to a restricted habitat, apparently shallow water.
At the end of the Eocene, and at the end of the deposition of the
L. (N.) chaperi zone, further shoaling probably occurred to the
extent that there was a period of mild erosion or at least non-depo-
sition. In Jackson County this probably did not proceed far enough
to bring the beds above water.
Marianna Limestone.-Renewed downsinking initiated deposi-
tion of the Marianna limestone in moderately shallow water. The
very fine chalky nature of the Marianna limestone in Jackson County
suggests that chemical precipitation was important in its formation.
Toward the end of the deposition of the Marianna limestone,
shoal conditions began to prevail once more. This brought to an end
the quiet, even deposition of the massive Marianna limestone, and
subaqueous scour and reworking occurred locally. The upper
portion of the section exposed at J-13 is indicative of this (figure
12).
Suwannee Limestone.-With the return to shallower conditions
Lepidocyclina (Eulepidina) spp. appeared with the deposition of
the Suwannee limestone. The trough to the east of Jackson County
may have remained more negative than the Marianna-Chipley area,
for a thicker Oligocene section is found there. This thickening may
be the result of post-Suwannee-pre-Tampa erosion in the Mari-
anna-Chipley area. Throughout the deposition of the Suwannee





GEOLOGY OF JACKSON COUNTY, FLORIDA


limestone the water was shallow. Minor fluctuations about an aver-
age depth produced good bedding and caused faunas to appear, dis-
appear, and reappear at different horizons at any given locality.
This may have resulted in part from structural movements and in
part from variations in the rate of sedimentation. Interbedded
marls, limestones, and sandy limestone suggest the same thing.
Miocene (Tampa).-At the end of the Oligocene, and probably
continuing into the Miocene, renewed uplift and faulting occurred
with the result that the Oligocene sediments were faulted and were
gently arched (plate III; figure 14). The top of this arch was eroded
before Miocene deposition occurred in central Jackson County.
On logs of two core holes at the Jim Woodruff Dam, W-1478,
and W-1479, Vernon expressed the opinion that the Oligocene-
Miocene contact at Chattahoochee was gradational. Along the Chi-
pola River the contact is not clear, but there seems to be no pro-
nounced unconformity. In the central portion of Jackson County
the Miocene beds cut across the bevelled surface of the Suwannee
limestone. The Cypress fault resulted from differential movement
between the positive block to the northwest and the negative block
to the southeast and its position may have been controlled by pre-
vious structure.
From the beginning of Miocene sedimentation to the deposition
of the Plio-Pleistocene formations in Florida, increasingly plastic
deposits were laid down. In going toward the northwest in Jackson
County, Miocene calcareous deposits become progressively scarcer
and clays become commoner. This indicates that the source of sedi-
ments was to the northwest. The depositional area to the east of
Jackson County remained relatively negative and thicker Miocene
deposits accumulated there. Faunas in the Tampa formation are
generally of the inner neritic type and the water at times must
have been very shallow. The green clay at elevation 135 feet at
the east end of the Jim Woodruf Dam on the Apalachicola River
appears to have been deposited over a mud-cracked surface. Tab-
ular flakes and fragments of the underlying white calcareous clay
were deposited in the bottom part of the green clay. Associated with
these flakes are many bone fragments including a manatee rib, fish
vertebrae, and freshwater fish breeding tubercles.3 These beds
represent marginal deposits of a delta which was being extended
into the Gulf of Mexico (Vernon, 1951, p. 184).

3Personal Conversation with Robert Ross and checked with E. C. Raney,
Cornell University, 1950.





FLORIDA GEOLOGICAL SURVEY


Post-Miocene.-Continued deposition extended this delta farther
into the Gulf of Mexico and culminated in deposition of the sands
and sandy clays that form the Delta Plain Highlands. Since that
time uplift, or a lowering of sea level, has raised these areas to
their present height.

Summary.-Central Jackson County has been a relatively posi-
tive area at least since upper Jackson time. Intermittent uplift
and slower sinking of this positive area coupled with dominant
downsinking of the negative area to the east and the south, has
resulted in the development of distinct lithologic and faunal facies.

ECONOMIC GEOLOGY

General.-Limestone, clay, sand, gravel deposits, and ground
water are the mineral resources of Jackson County that have a
proved occurrence in quantities great enough for commercial ex-
ploitation. Water alone is being exploited on a substantial scale.
Limestone is being produced in commercial quantities at only one
quarry, though minor operations for the production of "chimney
rock" occur sporadically. Sand in limited amounts is produced
within the county for use in concrete, but larger operations could
be sustained in the southern part of the county. Clay is being
utilized only in the preparation of roadbeds.

Clay.-The use of clay at the present time is limited to the con-
struction of highway roadbeds. The sandy clay or clayey sands of
the terrace deposits are preferred, because of their good permea-
bility. These sandy clays are generally secured from small borrow
pits.
Certain clays were used in the past for the manufacture of
brick, but no kilns are operating in the county today. Control of
the quality of the finished product was a serious difficulty en-
countered by these early brick manufacturers. Unsatisfactory kilns
and inadequate temperature control primarily were responsible for
the non-uniform product. In general the clays of the terrace de-
posits are most likely to be suitable for the manufacture of common
brick because most are lower in calcium carbonate and are less apt
to bloat during firing. Four clays in Jackson county are known to
be suitable for brick manufacture on the basis of past production
and laboratory tests. These are found at: 1. Locality J-183, 100
yards southwest from the road intersection in sec. 17, T. 4 N., R.
11 W.; 2. A pit on the grounds of the Florida Industrial School for





GEOLOGY OF JACKSON COUNTY, FLORIDA


Boys; 3. The old Blackman clay pit in the SE 14 sec. 6, T. 6 N., R.
12 W.; and 4. Locality J-162 located 100 yards south of the roid
corner in the SW 1/4 SE1/ NW 1/4 sec. 9, T. 3 N., R. 11 W. In Ap-
pendix II test data determined by the Florida Engineering and
Industrial Experiment Station are listed for clays typical of those
found in the county. These clays were selected for testing primarily
with reference to their geological occurrence so that some basis for
further exploration might be available. Test data for clays at lo-
calities J-183 and J-162 are included in Appendix II.

The pit at locality J-183 was operated formerly by Mr. Barbour
of Cottondale to produce clay for the manufacture of brick. The
property, now owned by Mr. J. P. Stanlind, has not been operated
for more than ten years. Brick made from this clay has a very
pleasing gray-white color and good physical properties (Appendix
II). It should also be noted that test data on this clay indicates
that it is suitable for use as a natural art pottery body, for use on
a wheel, and for use as a refractory clay. A brick of similar ap-
pearance was produced a good many years ago at the old Blackman
clay pit located in the SE 1/ sec. 6, T. 6 N., R. 12 W. Both the Bar-
bour and Blackman pits are located on low ground in beds within
the terrace deposits. These deposits of dark colored clay may repre-
sent accumulations in meander loops along the old streams that de-
posited the terrace materials. The altimeter elevation of the Black-
man pit is 152 feet and of the Barbour pit, 151 feet.

Clay from locality J-162, according to the test data, (Appendix
II) is suitable for the manufacture of common brick, hollow tile,
drain tile, and round tile. This locality is on an extensive terrace
flat, the Pamlico surface. The underlying bedrock is clay of the
Tampa formation.

Brick for some of the older buildings at the Florida Industrial
School for Boys was made from clay obtained on the school grounds.
The exact location of the old pit could not be determined, but it was
reported to have been located near the present highway, Fla. 276,
which would have placed it at a lower elevation than the surround-
ing terrain. The elevation of this clay pit probably was not below
115 feet. The Tampa formation-Suwannee limestone contact in
Well W-1824, located north of the highway at the Boys school, was
found to be at an elevation of 116 feet. The clay found in this pit
was probably derived from clays of the Tampa formation that were
leached relatively free of calcium carbonate.





FLORIDA GEOLOGICAL SURVEY


Exploration for Clay.-An analysis of past clay pit operations
and the tests performed by the Engineering and Industrial Experi-
ment Station, University of Florida, indicate that clays suitable
for the manufacture of brick and other fired ware are most likely to
be found underlying terrace surfaces. The best clays appear to
have been found on either the Pamlico or the Wicomico terraces,
and when these are underlain by clays of the Tampa formation
they offer the most promise.
Sand and Gravel.-Gravel is not abundant in commercial quan-
tities in Jackson County. One deposit was worked years ago. This
pit, located on the Henderson farm, 3.8 miles south of Cottondale on
Fla. Highway 75, at an altimeter elevation of 139 feet, produced
gravel composed of well rounded quartzite pebbles that ranged in
size from one to two inches in diameter. The one inch pebbles are
the most common. The gravel occurs in a red, micaceous clayey
sand, and is composed of badly fractured pebbles which are not
suitable for use in concrete subjected to high stresses.
Sand is abundant in most parts of the county, but it generally
requires washing to remove the clay if a high grade product is
desired. Large quantities of rather coarse sand can be obtained
in the Delta Plains Highlands of the southwestern part of the
county. This sand requires very little washing to obtain clean sand.
Limestone.-There is a sufficient quantity of limestone in Jack-
son County to sustain large commercial quarrying operations. In
the past the Crystal River limestone was quarried for use as road
base courses, and the Marianna limestone was quarried in the early
1800's for use as a building stone. Road base materials are used
from the most available and cheapest source and the Crystal River
is used only where it is available along or near a right of way. The
use of the Marianna limestone decreased as production costs, pri-
marily labor, increased, and today concrete blocks have replaced the
Marianna limestone as a building stone.
The only commercial limestone quarry operating in Jackson
County is owned by the Marianna Limestone Products Co. and is
situated near the center of Sec. 23, T. 5 N., R. 11 W. (loc. J-5). This
company produces crushed agricultural limestone from the Bump-
nose limestone.
The important properties of the Eocene limestones are their
softness, their high calcium carbonate content, and their low
magnesium content. These limestones are suitable for' many pur-





GEOLOGY OF JACKSON COUNTY, FLORIDA


poses: burnt lime products, cement, calcium carbonate fillers, and
chemical uses. The softness of these limestones offers several
advantages which have not been fully investigated. When dry,
these limestones can be ground to a very fine state with minimum
power; however, when wet, the limestone does not crush well and
tends to form a lime mud that clogs conventional hard-rock crushers.
If markets for sufficient crushed limestone can be obtained, new
quarrying and processing techniques seem justified. Portable roof
shelters might be used to protect the rock from the rain thus per-
mitting continuous operation of the crushers. Perhaps a large,
high capacity crusher can be developed that is able to handle soft
rock without serious clogging.

The Marianna limestone is available in quantity at the surface
only in the Marianna-Cottondale area. This limestone is one of the
earliest used building stones in Florida. The soft, compact, cream-
colored rock was sawed into blocks by cross cut saws for use in the
construction of buildings and chimneys. As labor cost increased,
the unit cost of the blocks became so high that now concrete blocks
are used instead of Marianna limestone. Because hand labor was
involved in the production of the limestone blocks, they were not
uniform. This fault gave a further advantage to the concrete block
industry. Untreated Marianna limestone is stained an unsightly
black on exposure by what is probably a fungus growth. While
not suitable for all types of construction, properly designed resi-
dence and two story buildings are sound and durable (figure 26).
The light color of the fresh stone is pleasing for architectural use
and the treatment of the stone to prevent the discoloration caused by
the fungus would enhance the beauty and possible sale of the blocks.
A most attractive residence, built by Mr. Cecil Rhyne of Marianna,
was built of Marianna limestone blocks faced with a ferruginous
sandstone (locally known as "iron rock") (figure 27).
Large reserves of high calcium Crystal River limestone and an
abundance of Miocene clays in Jackson County provide raw ma-
terials for cement manufacture.

Ground Water.-Ground water is plentiful in Jackson County,
and large quantities of water are generally produced from wells
that penetrate the bedrock. This water is normally uncontaminated
but is "hard" because of the presence of dissolved bicarbonates.
The Crystal River formation, the most important source of
ground water, lies at or near the surface in most of the county. The




86 FLORIDA GEOLOGICAL SURVEY



























Figure 26.--Community House, Marianna, Florida. This building is con-
structed of Marianna limestone.



















S./' 1








Figure 27.-The residence of Mr. Cecil Rhyne, Marianna, Florida. This
house is constructed of Marianna limestone blocks faced with ferruginous
sandstone.




GEOLOGY OF JACKSON COUNTY, FLORIDA


Suwannee limestone and the Tampa formation are also aquifers and
are very important sources of ground water in the southern part of
the county. The terrace sands of the Coharie formation are like-
wise important sources of water in the southeastern part of the
county. Most municipalities and industries obtain their water from
middle Eocene formations which are normally too deep for domestic
users.
Ground water in the Crystal River formation aquifer is artesian,
and water in wells that penetrate the aquifer rises to a level where
the column of water in the well balances the hydrostatic head.
The position of the water levels in wells in relation to the land sur-
face is controlled by the location of the well in the county, the
porosity of the aquifer, the elevation of the surface, the hydrostatic
head, and other hydraulic factors. In Jackson County these levels
generally lie 10-50 feet below the ground surface. Springs are
present in the lower portions of the county; some wells located in
these low places might flow.

Petroleum.-Three petroleum test wells, all dry and abandoned,
have been drilled in Jackson County. A number of stratigraphic
test wells have been drilled, and most of the county has been sur-
veyed by some geophysical means. The fact that the Marianna-
Chipley area is structurally high has been recognized for a number
of years, but results of petroleum exploration in this area have been
discouraging.
Oil is being produced in Florida at the Sunniland field from a
porous zone in evaporites and carbonates of Early Cretaceous age.
The oil production nearest Jackson County is at the Pollard field,
Escambia County, Alabama, and at the Gilbertown field in Choctaw
County, Alabama.
In re-examining the petroleum prospects of Jackson County, a
review of the conditions favorable for the occurrence of petroleum
in the earth's crust is in order. Pratt (1944, p. 1507) points out
that,

"... the primary desideratum continues to be a thick marine series
of rapidly accumulated, plastic, or saline sediments, rich in organic
matter."

The three deep petroleum test wells drilled in Jackson County in-
dicate that a thick section of marine rocks exists. Accumulation of
petroleum is dependent upon the existence of a trap and a suitable




FLORIDA GEOLOGICAL SURVEY


geometric arrangement of caprock and reservoir rock that will
localize the accumulation. It is the search for a trap that has been
most difficult in explorations for petroleum in Florida.
The Marianna-Chipley structural high is a regional feature
and any petroleum accumulations that may be found in this area
can be expected to be in smaller local traps located on this regional
structure. Past success in oil discovery in the eastern Gulf Coast
area suggests that Cretaceous formations offer the greatest promise
for petroleum production in Florida. These formations, in Jackson
County, lie at depths greater than 1937 feet (Cole, 1938). The
present report is concerned primarily with the surface and shallow
subsurface geology of Jackson County; the deeper Cretaceous beds
were not studied. A report being prepared by members of the
Survey on the Panhandle will include these rocks. A number of un-
conformities exist between formations exposed at the surface in
Jackson County and those occurring at depth, so that structures
present at the surface are not necessarily present at depth. How-
ever, structures present at the surface can contribute much to the
interpretation of deeper structures located by geophysical methods
or by stratigraphic drilling. Therefore, the following suggestions
are advanced with these limitations in mind.
One localized structure in Jackson County deserves mention as
a possible petroleum trap, the domed structure on the southeast,
or downthrown side, of the Cypress fault that closes against the
fault (figures 5, 6, 9). This structure and the fault appear to have
developed as a result of post-Suwannee-pre-Tampa stresses. The
depth to which this structural closure persists is unknown, and
it could not be determined from the data at hand whether there
was closure on the northwest, or upthrown, side of the fault. A
more complete description of this structure can be found on page 26.
A number of characteristics of the Marianna-Chipley area make
this structure interesting. The area long has been recognized as a
structural high and four oil test wells have been drilled in the area,
one in Washington County (W-l) and three in Jackson County
(W-285, W-1886, and W-2777).' How long the Marianna-Chipley
area has been a structurally positive area is unknown, but there
is the suggestion that this area was structurally positive at least
as early as Midway time, for Applin and Applin (1944, fig. 23, pp.
1736-1737) show a thinning of beds of Midway age and the absence
of beds of Navarro age at the Hammonds No. 1 Granberry well
(W-285) on their structure section. This well, W-285, is located on

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5927ec8bde480cf784c1309d45a7d1c7ec3e407c
'2012-05-16T11:58:57-04:00'
describe
'455557' 'info:fdaE20100110_AAACDNfileF20100110_AABNLS' 'sip-files00004.jp2'
86610dcfb08d37b7e05984693ed4eb82
5715ea4fcc51e70424ce4e2ede6f483208f287dd
'2012-05-16T11:57:20-04:00'
describe
'595240' 'info:fdaE20100110_AAACDNfileF20100110_AABNLT' 'sip-files00004.jpg'
063c2ca78b35d3c62a23b59084cc57e5
fde674d3fb34c9f9c6f8bf91af89acb03aa0c6d7
'2012-05-16T11:59:11-04:00'
describe
'65291' 'info:fdaE20100110_AAACDNfileF20100110_AABNLU' 'sip-files00004.pro'
4a9baa61600b3da1b86939c716d4beae
89aedf5b57d17eaffd7fc196ce44d1eb5f9e66bd
'2012-05-16T12:03:00-04:00'
describe
'187444' 'info:fdaE20100110_AAACDNfileF20100110_AABNLV' 'sip-files00004.QC.jpg'
3d119d8b58afd055d0e89a7ba3f88126
65a5b0aa56e4c7f9cad22a850bc83b6dd4bce508
'2012-05-16T12:06:05-04:00'
describe
'3647450' 'info:fdaE20100110_AAACDNfileF20100110_AABNLW' 'sip-files00004.tif'
ff3801fab539645743aa3d2debc01a5c
821ea42dc0e0e83733a06806aff53a99a10efccc
'2012-05-16T11:59:44-04:00'
describe
'2584' 'info:fdaE20100110_AAACDNfileF20100110_AABNLX' 'sip-files00004.txt'
53139e324d69b7083c28371dd2f319f9
646ad80958a6f1627a6059c7559c9a0bb73c3184
'2012-05-16T12:04:26-04:00'
describe
'51439' 'info:fdaE20100110_AAACDNfileF20100110_AABNLY' 'sip-files00004thm.jpg'
f0c4749578d3d68d91d92084dff73b1c
2148ed7d9cc744591ccce3b5a1f6896a72a7bbf6
'2012-05-16T11:57:23-04:00'
describe
'464355' 'info:fdaE20100110_AAACDNfileF20100110_AABNLZ' 'sip-files00005.jp2'
53d0e43178af55330867ce276d6fe95a
5a92033ca470245ca74d7ca5b60d5ae3c9f2446a
'2012-05-16T12:01:21-04:00'
describe
'589083' 'info:fdaE20100110_AAACDNfileF20100110_AABNMA' 'sip-files00005.jpg'
ae30cc8f06ba536986e1c7d001c27388
f0454e01bf6dc0facb89fa49c83d43aa9220abee
'2012-05-16T12:06:42-04:00'
describe
'65476' 'info:fdaE20100110_AAACDNfileF20100110_AABNMB' 'sip-files00005.pro'
ef4f75a9c2ebae4a575542cfebea3544
4dfe07d8cb990570b1d56bb6885ba521f15ee6af
'2012-05-16T12:05:34-04:00'
describe
'186174' 'info:fdaE20100110_AAACDNfileF20100110_AABNMC' 'sip-files00005.QC.jpg'
d917bdd1d9776332bdbbb83d17ca0e45
d8ef6e31a56083bdbfd3ea6a3db32c7f47730958
'2012-05-16T11:57:59-04:00'
describe
'3717234' 'info:fdaE20100110_AAACDNfileF20100110_AABNMD' 'sip-files00005.tif'
008471655bf129fa02d2bad64b399417
4b9a33677eff5d09141e5e32618612a25fb9eb80
'2012-05-16T11:56:06-04:00'
describe
'2595' 'info:fdaE20100110_AAACDNfileF20100110_AABNME' 'sip-files00005.txt'
0594eb7eb5d4a9141a515967cd80e52d
b705c55604f7436c816f542aaea75fc7246c7f4f
'2012-05-16T12:04:18-04:00'
describe
'52575' 'info:fdaE20100110_AAACDNfileF20100110_AABNMF' 'sip-files00005thm.jpg'
f02d38a58a14212eb82b299462a2827c
a9dc75c7faec8cb7be51fb6ffa7e59076aed16cb
'2012-05-16T12:02:53-04:00'
describe
'470811' 'info:fdaE20100110_AAACDNfileF20100110_AABNMG' 'sip-files00006.jp2'
490ccb3e4cf98ed4b09f4b13a39fe8aa
5bde23f8405bce75d0dd1917fe088db23459349e
'2012-05-16T12:04:27-04:00'
describe
'536960' 'info:fdaE20100110_AAACDNfileF20100110_AABNMH' 'sip-files00006.jpg'
b2a4b805366e1d62b3c58e5033419524
db8fcc9813d72b9ee7ea9eea9449f7be9779de82
'2012-05-16T12:00:57-04:00'
describe
'62964' 'info:fdaE20100110_AAACDNfileF20100110_AABNMI' 'sip-files00006.pro'
b9aa6f65844b4c165d399fbd7f18b592
556b66f3b41452dcb9d8fc9a805602b15c54fab1
describe
'169692' 'info:fdaE20100110_AAACDNfileF20100110_AABNMJ' 'sip-files00006.QC.jpg'
755e78231b8e6e4ae06622db4e672908
0153ecd1db0beba6e3793c171d51a1653d107cd6
'2012-05-16T12:03:37-04:00'
describe
'3769274' 'info:fdaE20100110_AAACDNfileF20100110_AABNMK' 'sip-files00006.tif'
3b6879cf89a5371f29e1fd21c174f0cd
e7d691bdc22ed7622c0ed8afd09bd8b3f9cc96e6
'2012-05-16T12:04:36-04:00'
describe
'2563' 'info:fdaE20100110_AAACDNfileF20100110_AABNML' 'sip-files00006.txt'
08437c9f4b17eec1beebf0ae7200ebd0
56da2d7eba55035cd3eea082b88b2acb58d676c2
'2012-05-16T11:59:29-04:00'
describe
'49546' 'info:fdaE20100110_AAACDNfileF20100110_AABNMM' 'sip-files00006thm.jpg'
e695d99310daec1eb1da4374e7071e56
10b19c91d4f23612a15b398cf68e7570f285859f
'2012-05-16T12:04:48-04:00'
describe
'486633' 'info:fdaE20100110_AAACDNfileF20100110_AABNMN' 'sip-files00007.jp2'
ea7bb060d7d2b0641ae1850b2aaa1ea9
422e8bfe24971f00d5ee7d22fe128c82a4f92136
'2012-05-16T12:04:10-04:00'
describe
'569505' 'info:fdaE20100110_AAACDNfileF20100110_AABNMO' 'sip-files00007.jpg'
0c71c22df50ecee5f370cea2313f6675
573cf716ed6ced0caf3752113670e5619b63f146
'2012-05-16T12:04:07-04:00'
describe
'68345' 'info:fdaE20100110_AAACDNfileF20100110_AABNMP' 'sip-files00007.pro'
04089b0b8306ca7923c576eb5ddd021a
5ef1b4918d4db6ef6777c717868f47cb51fff03f
'2012-05-16T11:59:58-04:00'
describe
'181955' 'info:fdaE20100110_AAACDNfileF20100110_AABNMQ' 'sip-files00007.QC.jpg'
9521d79a32655ca8eef68e3349cd30ed
b71e7be5d8ed3bfad01599c4a08b9c33e4d755d2
'2012-05-16T11:59:51-04:00'
describe
'3895640' 'info:fdaE20100110_AAACDNfileF20100110_AABNMR' 'sip-files00007.tif'
0062468fb32c29831be7f58d10d08d08
45f76cd63108bab6505a79af5f1c1eec167cf5ef
'2012-05-16T12:01:36-04:00'
describe
'2755' 'info:fdaE20100110_AAACDNfileF20100110_AABNMS' 'sip-files00007.txt'
c4f7f95fd0fd9a0d8b4c38217530bea3
c6476333146c9747489c8b310040da6c1316292a
'2012-05-16T12:03:20-04:00'
describe
'47779' 'info:fdaE20100110_AAACDNfileF20100110_AABNMT' 'sip-files00007thm.jpg'
ed26a479d4e9c79e78dfb8c2f9f21f3f
fa4a3d1977506f9a70191efaac5a9e9fad9d5f0c
'2012-05-16T12:04:45-04:00'
describe
'491606' 'info:fdaE20100110_AAACDNfileF20100110_AABNMU' 'sip-files00008.jp2'
7f3219a2e34d12d7bd456c57c6eef0b9
28c12f5d0a5c48816d651353ee92304143ada9d6
'2012-05-16T12:06:19-04:00'
describe
'582742' 'info:fdaE20100110_AAACDNfileF20100110_AABNMV' 'sip-files00008.jpg'
c11564ca5c285787bb5e1b414b342a2a
3ab569dece6d4affa1835ab5557e4db130f9b26a
'2012-05-16T12:02:49-04:00'
describe
'66298' 'info:fdaE20100110_AAACDNfileF20100110_AABNMW' 'sip-files00008.pro'
46ee289e5c2bc4181c47770e34600da0
b1b36d928eb1098baff228612f53e4527bd0dc03
'2012-05-16T11:58:10-04:00'
describe
'183928' 'info:fdaE20100110_AAACDNfileF20100110_AABNMX' 'sip-files00008.QC.jpg'
592636653b8ca5928375a7d57b5b05c4
d420164b758ff5830664e25d095ccc127cf5c40f
'2012-05-16T12:05:10-04:00'
describe
'3935492' 'info:fdaE20100110_AAACDNfileF20100110_AABNMY' 'sip-files00008.tif'
9ea57c4ed49abeacf9ac984eb69355e3
1ac23911ae1a0c74747ca813fb13dbed23dccc20
'2012-05-16T11:56:32-04:00'
describe
'2618' 'info:fdaE20100110_AAACDNfileF20100110_AABNMZ' 'sip-files00008.txt'
e33eeaf9f9896beee8570b4eecc47fc6
53900d1908a762eb9eec48c55b76d945531b8cb9
'2012-05-16T12:03:43-04:00'
describe
'48575' 'info:fdaE20100110_AAACDNfileF20100110_AABNNA' 'sip-files00008thm.jpg'
9e32740ee43199eb3d1b5d8c88f3ff40
d3916894fd6a1eeab3d1d3d50de6251a11b5f190
'2012-05-16T12:01:10-04:00'
describe
'472283' 'info:fdaE20100110_AAACDNfileF20100110_AABNNB' 'sip-files00009.jp2'
bbe1cd6ccfd90fccc69bb981714975db
7762a1dd933ae322e70365823e7d460832069ee3
'2012-05-16T11:57:25-04:00'
describe
'544354' 'info:fdaE20100110_AAACDNfileF20100110_AABNNC' 'sip-files00009.jpg'
96c9dba98f70507d23c5f9f0fd4136f8
9be6cdb35528ba49b8c747ba472dca797739c167
'2012-05-16T11:58:20-04:00'
describe
'65941' 'info:fdaE20100110_AAACDNfileF20100110_AABNND' 'sip-files00009.pro'
e225e327d97644b4a8e56d10e9612c0b
2697b22c5a577801b12eb856d7ab6015555f2420
'2012-05-16T11:56:55-04:00'
describe
'177151' 'info:fdaE20100110_AAACDNfileF20100110_AABNNE' 'sip-files00009.QC.jpg'
e9657968fb640043142c4bef1ab9c1fd
6abc2175ed4bdd3a873e90160fbc9ce3914aeb15
'2012-05-16T12:05:13-04:00'
describe
'3781314' 'info:fdaE20100110_AAACDNfileF20100110_AABNNF' 'sip-files00009.tif'
4589da747af9b8c42d9abaa24b15e478
b3632fce9977421e268ca982c41da725d4df0e25
'2012-05-16T12:05:36-04:00'
describe
'2609' 'info:fdaE20100110_AAACDNfileF20100110_AABNNG' 'sip-files00009.txt'
27dfb253ebf342be66a90ee9c4ced390
8d10b3018bfc85891248b2fd975d550e6133e5bd
'2012-05-16T11:58:04-04:00'
describe
'50576' 'info:fdaE20100110_AAACDNfileF20100110_AABNNH' 'sip-files00009thm.jpg'
331fe4958b58e108fd323466e8cc2ee9
fb8fab3fdc44b48ed0967c03f826544c64b0a996
'2012-05-16T11:57:28-04:00'
describe
'488181' 'info:fdaE20100110_AAACDNfileF20100110_AABNNI' 'sip-files00010.jp2'
8e8f109ce1c1de33b0f7daf910d1ab95
948803b92846d623ad198b953ebd641471ebbcde
'2012-05-16T12:01:23-04:00'
describe
'576035' 'info:fdaE20100110_AAACDNfileF20100110_AABNNJ' 'sip-files00010.jpg'
510fc0dd47c2cf37beab638b44d433c5
f2991cfe2275275fbdab9d6d24314ba81750a07e
'2012-05-16T12:00:50-04:00'
describe
'67569' 'info:fdaE20100110_AAACDNfileF20100110_AABNNK' 'sip-files00010.pro'
549c49d6760f4bd2b3d53a806c23e005
c520f9f6a438759c159cedaa6b42e5e06305727f
'2012-05-16T12:06:46-04:00'
describe
'181806' 'info:fdaE20100110_AAACDNfileF20100110_AABNNL' 'sip-files00010.QC.jpg'
c51d9fc5345c4d9f26e40b2d14b4d068
972ece67a32e50550e6e4d8697e2aed9817eff29
describe
'3908106' 'info:fdaE20100110_AAACDNfileF20100110_AABNNM' 'sip-files00010.tif'
990f651a8ea76d2b88acfcf6c3e84c4e
21aa1b42212c313de24dceea746cf38d8cd031cd
'2012-05-16T12:03:26-04:00'
describe
'2661' 'info:fdaE20100110_AAACDNfileF20100110_AABNNN' 'sip-files00010.txt'
36a12feb666df2f9e42e253b380fd985
2a50a82396852527c53a791e963f7c2e81fa18d3
'2012-05-16T12:04:33-04:00'
describe
'47825' 'info:fdaE20100110_AAACDNfileF20100110_AABNNO' 'sip-files00010thm.jpg'
7d3b5b7cc96a0b5e0dfc65823cbf20ec
b9d502e9996cb47ef878a1570b7260c4da471b89
'2012-05-16T12:06:04-04:00'
describe
'472332' 'info:fdaE20100110_AAACDNfileF20100110_AABNNP' 'sip-files00011.jp2'
50e8dee7ebf51d6272511b730e870bf2
8ef8468755225d6039a3decf5af667e1e25ab61d
'2012-05-16T12:07:07-04:00'
describe
'566963' 'info:fdaE20100110_AAACDNfileF20100110_AABNNQ' 'sip-files00011.jpg'
462f3095fd254b70148b1801797ff6da
cd4cd0b80fd830c8d344025ff704c232ea286477
'2012-05-16T12:06:00-04:00'
describe
'64984' 'info:fdaE20100110_AAACDNfileF20100110_AABNNR' 'sip-files00011.pro'
50a658626a57840d1efad67bb23b447b
7abac87bf111a1fea58459ab225f0cfe3fc097af
'2012-05-16T12:04:20-04:00'
describe
'181809' 'info:fdaE20100110_AAACDNfileF20100110_AABNNS' 'sip-files00011.QC.jpg'
927f61a1488c97848f643d510410bc0a
72741ace77163a8167e35df3b9e4364621d8a1d3
'2012-05-16T12:03:23-04:00'
describe
'3781154' 'info:fdaE20100110_AAACDNfileF20100110_AABNNT' 'sip-files00011.tif'
d4ab103896fef33c0362d2b98097008d
8b584965396e988a4b2ce8b431682f463652f49b
'2012-05-16T12:04:42-04:00'
describe
'2575' 'info:fdaE20100110_AAACDNfileF20100110_AABNNU' 'sip-files00011.txt'
75abb871bc5ff1a78dab38a7452bcc3b
1d5f5b3f498fed1e7b89fa8f1b8ef9dbe32392f9
'2012-05-16T11:56:31-04:00'
describe
'48131' 'info:fdaE20100110_AAACDNfileF20100110_AABNNV' 'sip-files00011thm.jpg'
93cc0ab1060edf23d50ceb3277175949
b128064ae64365feac9c9b660435f2b5795eacd5
'2012-05-16T11:57:24-04:00'
describe
'478962' 'info:fdaE20100110_AAACDNfileF20100110_AABNNW' 'sip-files00012.jp2'
21a9efb201d368471bd75d0cad96db5e
75bddb40e4890b614efcabd602c5294adb0b311a
'2012-05-16T11:57:26-04:00'
describe
'560319' 'info:fdaE20100110_AAACDNfileF20100110_AABNNX' 'sip-files00012.jpg'
8f5fd9d6a578e9a98ee0a81941f6abdb
a458de7069963113d2cc1fc886b2418d6d9db4fa
'2012-05-16T11:56:46-04:00'
describe
'66215' 'info:fdaE20100110_AAACDNfileF20100110_AABNNY' 'sip-files00012.pro'
7a5b16648f5b25b7b19bb541e6f1dcf6
05fac78db8e72484ecd46c84495960c0f0feaa37
'2012-05-16T12:05:35-04:00'
describe
'178790' 'info:fdaE20100110_AAACDNfileF20100110_AABNNZ' 'sip-files00012.QC.jpg'
136b8f34b6475f7c8efd657dd221e685
8958cafbea4fea242a45a92badf4a914842591f7
'2012-05-16T12:06:50-04:00'
describe
'3834124' 'info:fdaE20100110_AAACDNfileF20100110_AABNOA' 'sip-files00012.tif'
8fe4c063a342a90f4bb88258de6ccb46
b49f142274f38136165579c2dfa7739caf2c4d81
'2012-05-16T12:02:00-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABNOB' 'sip-files00012.txt'
6f20d32be3a06ebc4dfed7106f1e815d
40dc5b6a756224339664cb0b0c40a4e000dc1220
'2012-05-16T12:01:43-04:00'
describe
'46853' 'info:fdaE20100110_AAACDNfileF20100110_AABNOC' 'sip-files00012thm.jpg'
597096d1db28f7c0049fe99d9d6fb1ad
29108f1b4a0db520f4ce4d5d8a7314a6284c5cc4
'2012-05-16T11:59:06-04:00'
describe
'485939' 'info:fdaE20100110_AAACDNfileF20100110_AABNOD' 'sip-files00013.jp2'
f199dfba05d4737293a67e0c27e1f970
38965aab3a2dd961d48782d6e7c1370285bdc581
'2012-05-16T12:02:01-04:00'
describe
'563305' 'info:fdaE20100110_AAACDNfileF20100110_AABNOE' 'sip-files00013.jpg'
5daa6f7abca415e27dfeb3ba519da1e6
e207cef18155925241cc2d4880e64238433c68e0
'2012-05-16T12:02:33-04:00'
describe
'65847' 'info:fdaE20100110_AAACDNfileF20100110_AABNOF' 'sip-files00013.pro'
963e85396187ce0fa0a43b50c2b03e5e
fff18d0bea9cc2294eddad8a9f3cd7aaccb78a1f
'2012-05-16T12:02:50-04:00'
describe
'180536' 'info:fdaE20100110_AAACDNfileF20100110_AABNOG' 'sip-files00013.QC.jpg'
8fa33fd6588ce2bd56ba063a0239d28f
bf096ce96e8379a9c8a3ea0bc259d1fc305eeba4
describe
'3890018' 'info:fdaE20100110_AAACDNfileF20100110_AABNOH' 'sip-files00013.tif'
f90135a66c88ae04e48b1eec20cbf9eb
b7b60d56aa3685f3a4ded9fa99381d553322a46c
'2012-05-16T12:05:44-04:00'
describe
'2599' 'info:fdaE20100110_AAACDNfileF20100110_AABNOI' 'sip-files00013.txt'
1fda5c74a8dbb92d0435f3d230275865
20ece65aa9c4e5681557b6605e2eca5c78b3d246
'2012-05-16T12:02:47-04:00'
describe
'46710' 'info:fdaE20100110_AAACDNfileF20100110_AABNOJ' 'sip-files00013thm.jpg'
2c8f6fce4ce3233f00aad94125e28b3b
29150d2c8a71689a83cccb3b133c20f4733cae65
'2012-05-16T12:04:02-04:00'
describe
'471733' 'info:fdaE20100110_AAACDNfileF20100110_AABNOK' 'sip-files00014.jp2'
3add0d066fc0b377a1362d7534d2caae
3b577b507c49c90954dd013b9240cee032705a17
'2012-05-16T12:04:16-04:00'
describe
'562961' 'info:fdaE20100110_AAACDNfileF20100110_AABNOL' 'sip-files00014.jpg'
46e09af7434b695bf3fe2cf0fa2ff429
90907aaa1fad46b53ac4b4c66019bc9bdb2eb803
'2012-05-16T11:58:49-04:00'
describe
'63599' 'info:fdaE20100110_AAACDNfileF20100110_AABNOM' 'sip-files00014.pro'
023c193d2e36d2d9ebd814d762614999
a326b219a317e941acf6defd133f80547297bb3b
describe
'178208' 'info:fdaE20100110_AAACDNfileF20100110_AABNON' 'sip-files00014.QC.jpg'
d0c472e20dcbb048f8c1e0e8decdea8e
d50b433320a57b53462d68854edbe00b404454b8
'2012-05-16T12:02:44-04:00'
describe
'3776206' 'info:fdaE20100110_AAACDNfileF20100110_AABNOO' 'sip-files00014.tif'
c7f48120b12c843e133a335caa52e5a4
f9a74e933be6ad545620b769913db7c79711df66
'2012-05-16T12:07:05-04:00'
describe
'2514' 'info:fdaE20100110_AAACDNfileF20100110_AABNOP' 'sip-files00014.txt'
eb3180d9e46b86ad49be7fc68c715a23
8a81dab8b86dfa0b6e1309d05a8f47494d063466
'2012-05-16T12:02:40-04:00'
describe
'47373' 'info:fdaE20100110_AAACDNfileF20100110_AABNOQ' 'sip-files00014thm.jpg'
3f48dc1a2ba1fc6d113cfd8bd72276c6
d25c7b0bdd1d4e143fc8b310bfac94968776597b
'2012-05-16T11:57:30-04:00'
describe
'480056' 'info:fdaE20100110_AAACDNfileF20100110_AABNOR' 'sip-files00015.jp2'
8f670a0f705f05889968a85cc41a6ebc
d9894fd8a492317865e50034dcff142e75fe880d
'2012-05-16T11:56:45-04:00'
describe
'427152' 'info:fdaE20100110_AAACDNfileF20100110_AABNOS' 'sip-files00015.jpg'
67e8a7d279dbba41ee1cc826176f3f10
2d083808d6eb66031e33d25562576e574d6645a7
'2012-05-16T12:06:28-04:00'
describe
'28524' 'info:fdaE20100110_AAACDNfileF20100110_AABNOT' 'sip-files00015.pro'
0391c60c70997afd9f960b6a75e2594b
4d445a4630a3330a40878d9959afa3df2bcfaeea
'2012-05-16T12:03:13-04:00'
describe
'130494' 'info:fdaE20100110_AAACDNfileF20100110_AABNOU' 'sip-files00015.QC.jpg'
570bc794c66e020a98e96503799d6eb1
d39fa123de0ba4c66106eb09e595c04fb8d7e7d3
'2012-05-16T12:04:34-04:00'
describe
'3843434' 'info:fdaE20100110_AAACDNfileF20100110_AABNOV' 'sip-files00015.tif'
df00bea8660ae8ae8de8a41808c05b43
ab4a47cb64f3562e47424e3c57eb572fbd0c550e
'2012-05-16T11:56:57-04:00'
describe
'1137' 'info:fdaE20100110_AAACDNfileF20100110_AABNOW' 'sip-files00015.txt'
b04abf15005bf16db7c66422473ae00d
44c981fcbdc801e004bf19fa8ba2173262b879e5
'2012-05-16T12:07:01-04:00'
describe
'35889' 'info:fdaE20100110_AAACDNfileF20100110_AABNOX' 'sip-files00015thm.jpg'
e69886bf13bbc59e55f3c84221478a3d
540ac562c5d9487bac7fab10ed75f86ed8331126
'2012-05-16T12:04:19-04:00'
describe
'486190' 'info:fdaE20100110_AAACDNfileF20100110_AABNOY' 'sip-files00016.jp2'
a083c9413f0027c00d38d2abfe187008
8f923cf1b8943f893878ec6557dff72dd5ca28a6
'2012-05-16T12:00:10-04:00'
describe
'575812' 'info:fdaE20100110_AAACDNfileF20100110_AABNOZ' 'sip-files00016.jpg'
c3f8d6abf786b27021268625598a43a7
af74baa1bac3ec5c315571cc4fbfd964c84d288c
'2012-05-16T12:04:55-04:00'
describe
'69790' 'info:fdaE20100110_AAACDNfileF20100110_AABNPA' 'sip-files00016.pro'
58f8335062c4d8b20aeb7c2094c4cea4
301c82a77d4657c17c84a899d030f11e50ef41b9
'2012-05-16T11:56:58-04:00'
describe
'184322' 'info:fdaE20100110_AAACDNfileF20100110_AABNPB' 'sip-files00016.QC.jpg'
b0573d0d501e085c45ff5348292c49b1
7ca4e665e660137cb4838191bbbaa4e9eadc1e98
'2012-05-16T11:57:18-04:00'
describe
'3891874' 'info:fdaE20100110_AAACDNfileF20100110_AABNPC' 'sip-files00016.tif'
bdcafad99ea70627b0f72be5ad2ce545
ddf0acea595a424b2d977bbe71c941facd4ddc84
'2012-05-16T12:06:48-04:00'
describe
'2754' 'info:fdaE20100110_AAACDNfileF20100110_AABNPD' 'sip-files00016.txt'
a6482c5ad46edd6f5327582feb3b0dd8
5994eefaa1cf43bb58f984ce8ddeb7358f33e1e1
'2012-05-16T12:03:58-04:00'
describe
'46805' 'info:fdaE20100110_AAACDNfileF20100110_AABNPE' 'sip-files00016thm.jpg'
78cde350b20df4e62deff27313199480
de2857bebaf00b983daeef946f07f677894f0b93
'2012-05-16T12:03:40-04:00'
describe
'480660' 'info:fdaE20100110_AAACDNfileF20100110_AABNPF' 'sip-files00017.jp2'
eb550a838d7695239d9b14453a6507f3
9f21d4fcc5bd293db92ab9cf1fa13cf20fa80311
'2012-05-16T12:00:27-04:00'
describe
'514174' 'info:fdaE20100110_AAACDNfileF20100110_AABNPG' 'sip-files00017.jpg'
4b87793f63a36eaa5bf9070fade753c2
09286e232fdc1cfe9e00034f62b55551a07c983a
'2012-05-16T12:06:39-04:00'
describe
'34800' 'info:fdaE20100110_AAACDNfileF20100110_AABNPH' 'sip-files00017.pro'
8f5b5ee771b313f3545d547b4af0d26b
dabbdc28f552e7a2182657ff9da7d7086cf692f6
describe
'154982' 'info:fdaE20100110_AAACDNfileF20100110_AABNPI' 'sip-files00017.QC.jpg'
04585797a7e684351755aaa6cf59d304
ba3d8834c0c28bee35ab82006dcfe66f1d03e274
'2012-05-16T11:58:13-04:00'
describe
'3848474' 'info:fdaE20100110_AAACDNfileF20100110_AABNPJ' 'sip-files00017.tif'
59b23561dcbbfb25f3820ea31fded769
5fed9a752c870ce2300278705ff66da9d0aa5cdd
'2012-05-16T11:59:46-04:00'
describe
'1501' 'info:fdaE20100110_AAACDNfileF20100110_AABNPK' 'sip-files00017.txt'
afa3cdd31d378d82b6d71c6ccf94c155
57fd085308f88ef4a48fcde0bf7c423ccdb4ca47
'2012-05-16T12:04:01-04:00'
describe
'42005' 'info:fdaE20100110_AAACDNfileF20100110_AABNPL' 'sip-files00017thm.jpg'
4a458df41c4825371b3aa336b9383930
23df06af899e7594396b1cbe461a3b4b608b77e0
'2012-05-16T11:56:12-04:00'
describe
'473569' 'info:fdaE20100110_AAACDNfileF20100110_AABNPM' 'sip-files00018.jp2'
7055239b16fcf175ea70c2ea220ec2cf
e5a4539eec9acbac33ca2ef07b2921ebc288762b
'2012-05-16T12:02:51-04:00'
describe
'510435' 'info:fdaE20100110_AAACDNfileF20100110_AABNPN' 'sip-files00018.jpg'
428cab120f2227c34f4f421a25266e0e
b683ba72910151d38a32fdda5e08990b300cc5bb
'2012-05-16T12:01:16-04:00'
describe
'57131' 'info:fdaE20100110_AAACDNfileF20100110_AABNPO' 'sip-files00018.pro'
80249a050682bffd38cefe3826543f66
d414733bd75851e74cd059ae068d737772ad1c3e
'2012-05-16T12:02:28-04:00'
describe
'160564' 'info:fdaE20100110_AAACDNfileF20100110_AABNPP' 'sip-files00018.QC.jpg'
619fa8a33437e156125d15e1406dbedf
083b7ef52ed71ff95ba9a7c713364b00b6a570fc
'2012-05-16T12:03:22-04:00'
describe
'3791002' 'info:fdaE20100110_AAACDNfileF20100110_AABNPQ' 'sip-files00018.tif'
5972127a07d9a1ce2c42912fcc111df9
4b1be5a3c0044938703f5e6f9936e324dd69c167
'2012-05-16T11:56:01-04:00'
describe
'2469' 'info:fdaE20100110_AAACDNfileF20100110_AABNPR' 'sip-files00018.txt'
79ef63240c881667331036ea03571fbd
04f2cc54d94279487aa35d90f3b2bec9ae76d2e7
'2012-05-16T12:03:48-04:00'
describe
'43182' 'info:fdaE20100110_AAACDNfileF20100110_AABNPS' 'sip-files00018thm.jpg'
d9a3040c40d623787e74e3519fd8d71d
88ea7c41ed14ea8d79feffab71018f9759e54bde
'2012-05-16T12:04:17-04:00'
describe
'462112' 'info:fdaE20100110_AAACDNfileF20100110_AABNPT' 'sip-files00019.jp2'
331da10b64fe9e1752babd81b66abe21
d828e524deacadcd824a82fe0b59a6af7de95fb4
'2012-05-16T11:58:40-04:00'
describe
'368257' 'info:fdaE20100110_AAACDNfileF20100110_AABNPU' 'sip-files00019.jpg'
51f714756b54aae6deba88b770f98497
01c212548f19826fa421f59200104f737a518ec0
'2012-05-16T12:06:40-04:00'
describe
'20319' 'info:fdaE20100110_AAACDNfileF20100110_AABNPV' 'sip-files00019.pro'
0f1480e295d16fec54d061c21c3f708a
eba5ea593499537f125eac1b60c74abd8eb1f95f
'2012-05-16T12:06:24-04:00'
describe
'118754' 'info:fdaE20100110_AAACDNfileF20100110_AABNPW' 'sip-files00019.QC.jpg'
40d97464d72bb3b65d078e5e03779308
beb6a3d379843c13fe0ae47bd6d2592e567b5a23
describe
'3699320' 'info:fdaE20100110_AAACDNfileF20100110_AABNPX' 'sip-files00019.tif'
388831eeac07ce22dffe765fe4fc0d7c
0a21f8bfab19ddb8cfe30595eed71c8eb4da5a35
'2012-05-16T12:06:37-04:00'
describe
'1062' 'info:fdaE20100110_AAACDNfileF20100110_AABNPY' 'sip-files00019.txt'
6647cfcbd938c328a8d957dec796574e
767b7d19628d392062c0f8c8c2c66e43502ff283
'2012-05-16T11:56:19-04:00'
describe
'37161' 'info:fdaE20100110_AAACDNfileF20100110_AABNPZ' 'sip-files00019thm.jpg'
838cde0be919f609d0dc431078229856
3fce74330336ecb2accc55c081ed220f6c813f05
'2012-05-16T11:57:54-04:00'
describe
'487930' 'info:fdaE20100110_AAACDNfileF20100110_AABNQA' 'sip-files00020.jp2'
ecef6813af8068d27960a347eab85745
9c9d2e26dc84659664b537a88bb4c6539ee6f24c
'2012-05-16T12:03:44-04:00'
describe
'516950' 'info:fdaE20100110_AAACDNfileF20100110_AABNQB' 'sip-files00020.jpg'
b22497dbe1cb217e6f788a49542e5446
6dbbded8724edd559fac4a107935685a3a448392
describe
'59331' 'info:fdaE20100110_AAACDNfileF20100110_AABNQC' 'sip-files00020.pro'
9ed54b414ce4cc670a2a2580cef5091c
81b1e2994132b372ce7181cad53ce860cf7e3668
'2012-05-16T12:00:34-04:00'
describe
'167014' 'info:fdaE20100110_AAACDNfileF20100110_AABNQD' 'sip-files00020.QC.jpg'
2c1d6c10419f6592136d87e0f1d63c5e
9947b23849576ee3e2a0140b4f3e843ac4258755
'2012-05-16T12:04:31-04:00'
describe
'3906194' 'info:fdaE20100110_AAACDNfileF20100110_AABNQE' 'sip-files00020.tif'
d4609f7fcf433e4a6f1570136e68fa9d
937a47784d99e89c14a0ffbb2c39577efa97df81
'2012-05-16T11:57:34-04:00'
describe
'2364' 'info:fdaE20100110_AAACDNfileF20100110_AABNQF' 'sip-files00020.txt'
d28e527f72268dd76c75aab1f0f8cc65
4343805390db9ca088f7daad80a8849ae2604b6a
'2012-05-16T12:02:55-04:00'
describe
'43626' 'info:fdaE20100110_AAACDNfileF20100110_AABNQG' 'sip-files00020thm.jpg'
0b62971178fd7088bee087220bab62ff
db6441d4980ba6533f8d8f0bedf48546fc9d6b55
'2012-05-16T12:01:47-04:00'
describe
'486809' 'info:fdaE20100110_AAACDNfileF20100110_AABNQH' 'sip-files00021.jp2'
33cd942f4757496b9fdd40b62efd9800
49d8754721af78a5b189b7707c012dc588e62de0
'2012-05-16T11:56:40-04:00'
describe
'182216' 'info:fdaE20100110_AAACDNfileF20100110_AABNQI' 'sip-files00021.jpg'
ee76671a5ebe368c9ce62655801c258a
feaf3c515b4959a95cd993196aba5f643aa689af
'2012-05-16T12:01:06-04:00'
describe
'27765' 'info:fdaE20100110_AAACDNfileF20100110_AABNQJ' 'sip-files00021.pro'
39f6d906b0355f2b5f1aed78d7a5f6b4
79e5a8498fe5dfcc2411281fa65f5ecab4bc5d44
'2012-05-16T12:04:47-04:00'
describe
'65418' 'info:fdaE20100110_AAACDNfileF20100110_AABNQK' 'sip-files00021.QC.jpg'
aea752ed8b95bd27bc344455a1fbedbc
7fbeca16a30a42f15e1bf8786cabe9880b4832df
'2012-05-16T11:59:23-04:00'
describe
'3882588' 'info:fdaE20100110_AAACDNfileF20100110_AABNQL' 'sip-files00021.tif'
1894ca58df92c606b1712e36708f5e38
77a52ddaac5b94faaf105ae68e25ee1fa2be1791
'2012-05-16T11:56:13-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABNQM' 'sip-files00021.txt'
83a4e46beb9f7ca9fd0b95d75c41e100
5b3095410396a7d85e3e44147e96cbcdbcb6a062
describe
'27485' 'info:fdaE20100110_AAACDNfileF20100110_AABNQN' 'sip-files00021thm.jpg'
a14e618fd1bfa8a79d3581b3ac0be9ce
6b68d697bd8173c1491d708cfb5731e8746fe0ef
'2012-05-16T12:04:06-04:00'
describe
'481812' 'info:fdaE20100110_AAACDNfileF20100110_AABNQO' 'sip-files00022.jp2'
0eba0cbaf6a112219d420d5e5ff7ca6f
c0e807218cc2f9c209c5d9376dd767d5edb9e796
'2012-05-16T12:04:29-04:00'
describe
'565415' 'info:fdaE20100110_AAACDNfileF20100110_AABNQP' 'sip-files00022.jpg'
0d2dfa11cf6779c7364d7622ef9bddeb
232277e92fd8d6f3abb4be643cf7fa3cd36dd4e6
'2012-05-16T12:02:29-04:00'
describe
'66354' 'info:fdaE20100110_AAACDNfileF20100110_AABNQQ' 'sip-files00022.pro'
9496b2acbbbdbd425d59af2b736c204e
17704a90d07251b428015d19220c1d7b1bce6e26
'2012-05-16T12:06:20-04:00'
describe
'178535' 'info:fdaE20100110_AAACDNfileF20100110_AABNQR' 'sip-files00022.QC.jpg'
34bba45db8ff8acead070c93667b128a
df003ac88463b507a9fa792f6525961a38d55e11
'2012-05-16T12:02:22-04:00'
describe
'3856914' 'info:fdaE20100110_AAACDNfileF20100110_AABNQS' 'sip-files00022.tif'
585578d90785a5df264bda827fc40acd
c10dec9ff8f62168d1d009cb2e063de26c938053
'2012-05-16T12:02:43-04:00'
describe
'2624' 'info:fdaE20100110_AAACDNfileF20100110_AABNQT' 'sip-files00022.txt'
5f7722cdc50e5944fa2fe098ec840da9
1e7f9232a68e97315d7e775dc3e5b522b67bc17f
'2012-05-16T11:58:35-04:00'
describe
'47311' 'info:fdaE20100110_AAACDNfileF20100110_AABNQU' 'sip-files00022thm.jpg'
3072dfcf3db5d896ef0bb51d4030427c
079f41f2fd4b7d08fabd2e40250741f185561b1f
describe
'488160' 'info:fdaE20100110_AAACDNfileF20100110_AABNQV' 'sip-files00023.jp2'
5aff8f8c889897855bbb7c28d7dc2867
d699002f3f81f13d1dee7a91e83d743214313385
'2012-05-16T12:02:18-04:00'
describe
'539112' 'info:fdaE20100110_AAACDNfileF20100110_AABNQW' 'sip-files00023.jpg'
697b130fe6ddf24f7e0bfba7d3a1ea2d
58b4b17ac29acb4a85d1cd4e8f6906d079e028df
'2012-05-16T12:01:52-04:00'
describe
'58600' 'info:fdaE20100110_AAACDNfileF20100110_AABNQX' 'sip-files00023.pro'
8076489d994b0408a082691aa3e62a90
c9d2c2626c4e8b93a455b54e3239a7410a650fff
'2012-05-16T12:03:50-04:00'
describe
'171979' 'info:fdaE20100110_AAACDNfileF20100110_AABNQY' 'sip-files00023.QC.jpg'
bde8a144787664b4c199a5cd8794642b
10b2853b29eebb1826b3d7262ee45ee76694b7d9
'2012-05-16T11:59:13-04:00'
describe
'3908090' 'info:fdaE20100110_AAACDNfileF20100110_AABNQZ' 'sip-files00023.tif'
9c255b8b28f22a72df0542dc47dbabcd
248d7f510a2bc6e838e3fd317dd54d7419cd6b8c
'2012-05-16T12:02:31-04:00'
describe
'2363' 'info:fdaE20100110_AAACDNfileF20100110_AABNRA' 'sip-files00023.txt'
e70deaf76f48e9aca17d4d02ef507322
f8c195a49995a9049f7182b55cd463af3adf0939
'2012-05-16T12:05:22-04:00'
describe
'44518' 'info:fdaE20100110_AAACDNfileF20100110_AABNRB' 'sip-files00023thm.jpg'
b65631d330bc9a4996bc0c83c57b4944
2db3ee4ae18a9ccceb0b0693b53713a1047a8e5e
'2012-05-16T12:01:41-04:00'
describe
'482475' 'info:fdaE20100110_AAACDNfileF20100110_AABNRC' 'sip-files00024.jp2'
e236238b8d8d7c49ad75f845abeb7143
cc41d9acdfe61ed995dd4df93ca0f8cc7aefd397
'2012-05-16T11:57:35-04:00'
describe
'553819' 'info:fdaE20100110_AAACDNfileF20100110_AABNRD' 'sip-files00024.jpg'
546346e04b74df5fea8d3f7d66c85e56
e2361adeb99195422b502565e4fa9a4dc16f3bba
describe
'65016' 'info:fdaE20100110_AAACDNfileF20100110_AABNRE' 'sip-files00024.pro'
2d927225f1877e3a2e7db0755717c6c0
3dc12542181b6e80e52dab8f1aea7fe6261be0f6
'2012-05-16T12:02:37-04:00'
describe
'171401' 'info:fdaE20100110_AAACDNfileF20100110_AABNRF' 'sip-files00024.QC.jpg'
0fcd26345685daf54938d4553c8544e9
132a7b855a821dc3a4e14326f1609c2ad1a0d593
'2012-05-16T12:06:18-04:00'
describe
'3862274' 'info:fdaE20100110_AAACDNfileF20100110_AABNRG' 'sip-files00024.tif'
93c74aede39fbc4b2e5d33044f63600b
9f6d967b1f90d7096cd8ee0d53cb1a99e3bc5790
'2012-05-16T12:06:14-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABNRH' 'sip-files00024.txt'
ae85cc79beced91814b977a2f0a34f8b
481debd28a6e1d4ef879ceb2d61429265c965c5a
'2012-05-16T11:58:46-04:00'
describe
'44791' 'info:fdaE20100110_AAACDNfileF20100110_AABNRI' 'sip-files00024thm.jpg'
03ba2676ff88781737334bfc83cf88bc
0ded971bc428a3e661b96a4a1904e5dd40385dc3
'2012-05-16T12:03:46-04:00'
describe
'470697' 'info:fdaE20100110_AAACDNfileF20100110_AABNRJ' 'sip-files00025.jp2'
526769a3242a178061981796e6f076f1
ef9a5f2b61ec6fdf1e32264e8cd6918b80a51df2
'2012-05-16T11:57:52-04:00'
describe
'593498' 'info:fdaE20100110_AAACDNfileF20100110_AABNRK' 'sip-files00025.jpg'
33e9b1217e357db28d377c944168f77e
78530b573503db9a60a18862aa62616747934b57
describe
'70075' 'info:fdaE20100110_AAACDNfileF20100110_AABNRL' 'sip-files00025.pro'
99120779611b1e2bfc667aeb16bcbf3f
3aab4e252f90e7ae5b61adbf745a6f604f1e27c8
'2012-05-16T12:05:38-04:00'
describe
'191554' 'info:fdaE20100110_AAACDNfileF20100110_AABNRM' 'sip-files00025.QC.jpg'
86ed11edb624da378a37b48ad20bfc7f
bf2c25b77794a4bb10b99cbf06b79f29f4dc9f96
'2012-05-16T12:02:23-04:00'
describe
'3767946' 'info:fdaE20100110_AAACDNfileF20100110_AABNRN' 'sip-files00025.tif'
e681c8983c86fc433af4fdfba23ea79e
59e9964ead7899865b5d5f8572d6d1fe5c7557d7
'2012-05-16T12:05:06-04:00'
describe
'2761' 'info:fdaE20100110_AAACDNfileF20100110_AABNRO' 'sip-files00025.txt'
cdbaebcdde3fd8e7e19d0e6e7305d96f
567f488084b67b163fd6ee5745eec0391e38ef1a
'2012-05-16T12:03:45-04:00'
describe
'50161' 'info:fdaE20100110_AAACDNfileF20100110_AABNRP' 'sip-files00025thm.jpg'
730516eaf478c9368e3968c63c29875a
db27e10b6031c688f8b1d68241c7fe1a58c23f1e
'2012-05-16T12:04:12-04:00'
describe
'486178' 'info:fdaE20100110_AAACDNfileF20100110_AABNRQ' 'sip-files00026.jp2'
ca1116ff1af08a4c5965d462298388f5
7e5bb1b49181c8fb28975f44a95cbf120d3d0a74
'2012-05-16T12:06:26-04:00'
describe
'545632' 'info:fdaE20100110_AAACDNfileF20100110_AABNRR' 'sip-files00026.jpg'
c843e7e1b787d78c59504cc68fe2d1e2
c50ae4a4cfa71899b406993f49601db6e3bf6012
describe
'61114' 'info:fdaE20100110_AAACDNfileF20100110_AABNRS' 'sip-files00026.pro'
2539df01c589fe2927d5c23fd9fba5b6
4f503ac8d21c7699df221e11e3dd369d19a388f3
'2012-05-16T12:03:52-04:00'
describe
'175235' 'info:fdaE20100110_AAACDNfileF20100110_AABNRT' 'sip-files00026.QC.jpg'
58ac6fde564d7122d245106a3f5c2580
e66178c58b64587c20cc0346e9e54d6b60800431
describe
'info:fdaE20100110_AAACDNfileF20100110_AABNRU' 'sip-files00026.tif'
690121d0cb86596bad51904b79b5f445
c7c9772ca49a5dfbe09506cbc1736c0580915bbd
'2012-05-16T12:01:58-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABNRV' 'sip-files00026.txt'
10b67677b72677223a7ae8ec4aa99d1d
92fc88b0a4a6c9f21e4bc7cfb5c1a13533683de6
'2012-05-16T12:02:24-04:00'
describe
'46190' 'info:fdaE20100110_AAACDNfileF20100110_AABNRW' 'sip-files00026thm.jpg'
1ce5655301ec5acf3992a767294d8b95
31595c06cdcd92e1116a0e825c4c050551afcb07
describe
'486406' 'info:fdaE20100110_AAACDNfileF20100110_AABNRX' 'sip-files00027.jp2'
3e56bb705a47d18e7c689208369f9311
2f76f7e8da6eb24ff2025e557dd9782ed4774f99
describe
'192631' 'info:fdaE20100110_AAACDNfileF20100110_AABNRY' 'sip-files00027.jpg'
98063d16991c5d6df74997987477b4bd
43ea296ddf0b8644c5a112ca105ec35bfed87549
'2012-05-16T12:03:21-04:00'
describe
'9787' 'info:fdaE20100110_AAACDNfileF20100110_AABNRZ' 'sip-files00027.pro'
98296d169fb5d5d6135be4a37211170e
b33b8630b97e712982b71b99865d3311d0df85cb
'2012-05-16T12:05:32-04:00'
describe
'68064' 'info:fdaE20100110_AAACDNfileF20100110_AABNSA' 'sip-files00027.QC.jpg'
2426df9d9603c738744ae294f179cec2
2580a7e9febcaf31db9c817eec97f90081052240
'2012-05-16T12:01:02-04:00'
describe
'4063166' 'info:fdaE20100110_AAACDNfileF20100110_AABNSB' 'sip-files00027.tif'
aec611be15ef1e22d6cdf79f7b0bf10c
ae9a2d011f95af1493fd38e171a9a51ab4fd023f
'2012-05-16T12:05:25-04:00'
describe
'499' 'info:fdaE20100110_AAACDNfileF20100110_AABNSC' 'sip-files00027.txt'
b9b209e5d7fdb2a66d658f45ebf9c4e5
07ec02bdd69016d79fc2fc46123ff1536e63bd3f
'2012-05-16T12:05:55-04:00'
describe
'27818' 'info:fdaE20100110_AAACDNfileF20100110_AABNSD' 'sip-files00027thm.jpg'
8743b8dabd07318f57b0153ced8b5cf6
de5435431d32faabe8872897ea0321a992cd11c3
'2012-05-16T11:57:08-04:00'
describe
'488578' 'info:fdaE20100110_AAACDNfileF20100110_AABNSE' 'sip-files00028.jp2'
c5ceebe30a82ef5d7aed70b892a1f3dc
92564fdc6c77cefac4d3ee311d91f5d0fcb5428b
'2012-05-16T11:59:22-04:00'
describe
'175095' 'info:fdaE20100110_AAACDNfileF20100110_AABNSF' 'sip-files00028.jpg'
eb58775f10856dac9f39eaa71793d71a
9c65bff3082caec095217ed2f3d606dcadb6b900
describe
'10421' 'info:fdaE20100110_AAACDNfileF20100110_AABNSG' 'sip-files00028.pro'
e93c64650c8d57c6c223d8e70fde2aa2
1af48a75945bf439f9009b1331ac1f7b987a7d50
'2012-05-16T12:00:22-04:00'
describe
'62954' 'info:fdaE20100110_AAACDNfileF20100110_AABNSH' 'sip-files00028.QC.jpg'
d8e1538d3c3bce57543e4d8899d81ac7
fa42d2ffd08a4abdddce8b6af881d3fdfd2aac75
'2012-05-16T12:01:54-04:00'
describe
'3839942' 'info:fdaE20100110_AAACDNfileF20100110_AABNSI' 'sip-files00028.tif'
72e126c55b9cb04c75393a4157abacd9
3974845a316b7f52a3b5b961b7e7a9d633d8c170
'2012-05-16T12:00:45-04:00'
describe
'540' 'info:fdaE20100110_AAACDNfileF20100110_AABNSJ' 'sip-files00028.txt'
e5a86fbaaa86a758ea035dda651a7eb4
326d99200104099ebdfb8c6bd5920ffc15bb4920
'2012-05-16T12:06:38-04:00'
describe
'26571' 'info:fdaE20100110_AAACDNfileF20100110_AABNSK' 'sip-files00028thm.jpg'
5d6f447c3078b8ab25a25cdb5263daf2
669c49568c4ae63d06d54b799609519f355490a7
'2012-05-16T11:58:12-04:00'
describe
'475956' 'info:fdaE20100110_AAACDNfileF20100110_AABNSL' 'sip-files00029.jp2'
fd6c68011fc6511c0cdb02bcc8566c66
2805798696fa55427adafac7bfe653cc6bb01ab5
'2012-05-16T11:57:36-04:00'
describe
'569237' 'info:fdaE20100110_AAACDNfileF20100110_AABNSM' 'sip-files00029.jpg'
942dcc5c3547ccac37c2957030d5712a
f780c3aec6352ffeed9901e44a48855edc9546a9
'2012-05-16T12:01:39-04:00'
describe
'65203' 'info:fdaE20100110_AAACDNfileF20100110_AABNSN' 'sip-files00029.pro'
c0626d2269e7f79d8cf4939eec07aff1
d4e819cde83e1f3a558a632528ac4dc1cb559e9a
'2012-05-16T12:05:17-04:00'
describe
'181588' 'info:fdaE20100110_AAACDNfileF20100110_AABNSO' 'sip-files00029.QC.jpg'
3c01413dfff2bbbf0878d9c02227f870
ff6d8467c64e39c7ce1f70976e69d4ff11b290d9
'2012-05-16T11:57:00-04:00'
describe
'3810106' 'info:fdaE20100110_AAACDNfileF20100110_AABNSP' 'sip-files00029.tif'
fda6ff95f43ac5a05c27f31a989b6069
dca30e71cc015c8d3b70bf9941a0657181c028f9
describe
'2598' 'info:fdaE20100110_AAACDNfileF20100110_AABNSQ' 'sip-files00029.txt'
e7ec4f9f0be0cee781c7bd0c246ccdd0
0f4d24a653e0130bc9516ea00b520454ebb29041
'2012-05-16T12:02:38-04:00'
describe
'47443' 'info:fdaE20100110_AAACDNfileF20100110_AABNSR' 'sip-files00029thm.jpg'
43ae8709292fa8fdcbf49f3e7d2e8a7e
293c4f3ae34b5f880e919946603af41fdc4f6599
'2012-05-16T11:57:07-04:00'
describe
'482667' 'info:fdaE20100110_AAACDNfileF20100110_AABNSS' 'sip-files00030.jp2'
75d82eedc34f653512cdcaa3cbc5c54c
b1ff00438d6262298902253895e112538dbc61b8
'2012-05-16T11:57:55-04:00'
describe
'602282' 'info:fdaE20100110_AAACDNfileF20100110_AABNST' 'sip-files00030.jpg'
088ea87630310ce9a1636bae9f86d92c
aac2967d60c87cb0650f5fb4108097b851362f3f
'2012-05-16T11:59:07-04:00'
describe
'66600' 'info:fdaE20100110_AAACDNfileF20100110_AABNSU' 'sip-files00030.pro'
631a27b512c7ae1f92562134538f520b
caa725e0677c4c196f34ed1b196ba49f773296d3
'2012-05-16T11:56:43-04:00'
describe
'192034' 'info:fdaE20100110_AAACDNfileF20100110_AABNSV' 'sip-files00030.QC.jpg'
e1b0ac6f09d1b19d927f021c9be0a405
d35c879ceb00d3325df2c454644b9f25e8de5833
'2012-05-16T12:03:57-04:00'
describe
'3864234' 'info:fdaE20100110_AAACDNfileF20100110_AABNSW' 'sip-files00030.tif'
b49b67a8291f25c4efae0f8679717e2c
97d61986b9ffdba78d6a41ab4ca04d4876c1e9e7
describe
'2645' 'info:fdaE20100110_AAACDNfileF20100110_AABNSX' 'sip-files00030.txt'
40de995005a403169ca10301898e7a60
44baf8b5cb8a2549fa0dee7af53820053acc2e9d
'2012-05-16T11:56:11-04:00'
describe
'48812' 'info:fdaE20100110_AAACDNfileF20100110_AABNSY' 'sip-files00030thm.jpg'
20c0e415b534cdcb923f95a445b582ea
34e678b3b4710b10bb75e601092839254521bf4f
'2012-05-16T11:59:38-04:00'
describe
'475261' 'info:fdaE20100110_AAACDNfileF20100110_AABNSZ' 'sip-files00031.jp2'
c5ed36861951487c9b425a3bd40f1496
3e97f39335dce34cfd549073a8686cfacd861d2e
'2012-05-16T12:03:14-04:00'
describe
'602598' 'info:fdaE20100110_AAACDNfileF20100110_AABNTA' 'sip-files00031.jpg'
55ba2f2fed9aab36f95c0bdbe8f5cf7f
5fe5d5251944c1c4c38ad82de625eefdcc370997
'2012-05-16T12:05:50-04:00'
describe
'64101' 'info:fdaE20100110_AAACDNfileF20100110_AABNTB' 'sip-files00031.pro'
8848982fe610588e4eba2ea6b71971e7
998eccfba6183d5217afe5604fe6f296b56a237f
describe
'188146' 'info:fdaE20100110_AAACDNfileF20100110_AABNTC' 'sip-files00031.QC.jpg'
024f080b703ddb39e2f2dbc1fb6f819b
9cd44447d418290baf1a9a0a8de1cb54fe646428
'2012-05-16T12:06:07-04:00'
describe
'3805098' 'info:fdaE20100110_AAACDNfileF20100110_AABNTD' 'sip-files00031.tif'
d3d83d7bd014ac7a83b0a6040020dcca
38ec7a0d55853072713f73fd59188341db3ed10e
'2012-05-16T11:56:09-04:00'
describe
'2534' 'info:fdaE20100110_AAACDNfileF20100110_AABNTE' 'sip-files00031.txt'
b1cb3bb9797a7ee04ad4fd999e24bf66
370af553440c079887eed54c66917c8a15c2e610
'2012-05-16T11:56:48-04:00'
describe
'48365' 'info:fdaE20100110_AAACDNfileF20100110_AABNTF' 'sip-files00031thm.jpg'
c24d656a4b1dc28603395d1db33a3d78
bdcd6625dfe43b9c4743b1a4d63fbf74ee3694e7
'2012-05-16T12:05:20-04:00'
describe
'488212' 'info:fdaE20100110_AAACDNfileF20100110_AABNTG' 'sip-files00032.jp2'
004264eaa7700a62e8710809bdb919b6
19eeb385bffdbdeb27846c232e9a0cfb40a4a8e0
'2012-05-16T12:04:35-04:00'
describe
'540827' 'info:fdaE20100110_AAACDNfileF20100110_AABNTH' 'sip-files00032.jpg'
6486c7b4e502f4b65b84fe02239fbffd
bbdd75c9229556a13748654d95df22ce769d90ed
'2012-05-16T11:58:18-04:00'
describe
'60712' 'info:fdaE20100110_AAACDNfileF20100110_AABNTI' 'sip-files00032.pro'
3eb67985e119eddf588a4c39a58ca32c
c5277ceb4a2784d724cf59b7dc3c67bd85c70995
describe
'172188' 'info:fdaE20100110_AAACDNfileF20100110_AABNTJ' 'sip-files00032.QC.jpg'
dec965738432e328c643e9ec1a9d5b2d
d8f8f04f1598b667d48b53816462e06d865baeec
'2012-05-16T12:04:51-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABNTK' 'sip-files00032.tif'
6a13189100ba5298d4b9a0b21ca34666
d141fc996822556cc3adae973a442a49222c3ddc
'2012-05-16T11:58:44-04:00'
describe
'2401' 'info:fdaE20100110_AAACDNfileF20100110_AABNTL' 'sip-files00032.txt'
f8c8543529b7b0e97031cc25b0a7fda1
4674ea99dd7122d5d039b839e21f11fef104d681
'2012-05-16T11:56:47-04:00'
describe
'46109' 'info:fdaE20100110_AAACDNfileF20100110_AABNTM' 'sip-files00032thm.jpg'
6b697dd94407d424f1fb210bbee9df45
7fc19447d490d24cdb23e2f8da91dc74e151e5ad
'2012-05-16T11:57:46-04:00'
describe
'484240' 'info:fdaE20100110_AAACDNfileF20100110_AABNTN' 'sip-files00033.jp2'
075176a1458dcc20b2824d9f06499287
c90a6d8955ad9503c12d61284965b8bda6b317fa
'2012-05-16T12:05:56-04:00'
describe
'434808' 'info:fdaE20100110_AAACDNfileF20100110_AABNTO' 'sip-files00033.jpg'
d7eddc6406d96bdc41cacabc93f2a67c
3b83c00c0f91d1190f99ec684e3f0b4ab9565d59
describe
'55303' 'info:fdaE20100110_AAACDNfileF20100110_AABNTP' 'sip-files00033.pro'
a838a5d98a04bc87d5232ee5d8a42f24
4abd2d52758a0e0aae27a70165b12c09513227e1
'2012-05-16T12:05:58-04:00'
describe
'129660' 'info:fdaE20100110_AAACDNfileF20100110_AABNTQ' 'sip-files00033.QC.jpg'
a15bf709e3dd4098f1dbd73a9201b126
cdcc8b3108d13226e755804c8179325a91a39f83
'2012-05-16T11:58:41-04:00'
describe
'3877718' 'info:fdaE20100110_AAACDNfileF20100110_AABNTR' 'sip-files00033.tif'
d0d750e2672664c8593fdb27caf465aa
e3056e357102b0d915c3e051604a1234d8a16690
'2012-05-16T12:06:21-04:00'
describe
'3102' 'info:fdaE20100110_AAACDNfileF20100110_AABNTS' 'sip-files00033.txt'
19c6bfbf68154cd2ad38b9374ac2225d
85ad152eb687f3c70d4798e4b90d37ad7bdcb0e1
'2012-05-16T12:04:28-04:00'
describe
'36280' 'info:fdaE20100110_AAACDNfileF20100110_AABNTT' 'sip-files00033thm.jpg'
1ae0b32677f849f4e0c8837d17ecd301
9cbcbda2fc96455876273f04c2c66c318c434f55
'2012-05-16T11:58:09-04:00'
describe
'485658' 'info:fdaE20100110_AAACDNfileF20100110_AABNTU' 'sip-files00034.jp2'
17be1cffa272cdd739d28140790f88b6
6024c5fdb77668d11cbefa957de6eb244686c3c5
'2012-05-16T12:03:59-04:00'
describe
'433170' 'info:fdaE20100110_AAACDNfileF20100110_AABNTV' 'sip-files00034.jpg'
a908bdc33571abcaa587d5cc226a019b
03fe176eafddac69c6e136cd9c2a9b7e148651be
'2012-05-16T11:58:07-04:00'
describe
'56726' 'info:fdaE20100110_AAACDNfileF20100110_AABNTW' 'sip-files00034.pro'
2891cb9eeb2b68402c542c86ea607d2b
9c93fac0110b2cfa5e38a128ff7cfe9e0589e15b
'2012-05-16T11:59:50-04:00'
describe
'134376' 'info:fdaE20100110_AAACDNfileF20100110_AABNTX' 'sip-files00034.QC.jpg'
0a78ecb2dc625ce29ff1f2432066988f
cda7aa156d8a8fc6156faea443b9ce49f358423d
'2012-05-16T11:56:35-04:00'
describe
'3887674' 'info:fdaE20100110_AAACDNfileF20100110_AABNTY' 'sip-files00034.tif'
ff2e5e1a82b1bf40264e6d538d6d0afc
30c9057b32af21821ea8158ed17179bbf36b8f20
'2012-05-16T12:03:17-04:00'
describe
'2964' 'info:fdaE20100110_AAACDNfileF20100110_AABNTZ' 'sip-files00034.txt'
69b69613451b30b47af1b921c930f3eb
b66d1076fcababae9a87f33114a81e80c93512e2
'2012-05-16T12:07:00-04:00'
describe
'37684' 'info:fdaE20100110_AAACDNfileF20100110_AABNUA' 'sip-files00034thm.jpg'
02be3317ed128f315b6ce5d1d1e50f26
a4a37d8300b9fba9af676fb82f1243a58c2b1a41
'2012-05-16T12:01:53-04:00'
describe
'468377' 'info:fdaE20100110_AAACDNfileF20100110_AABNUB' 'sip-files00035.jp2'
d45e30d93e84c1f71206ddec4ae0325e
1ed8549da35572d900cb9528ce4af3dc6306ef3a
'2012-05-16T12:04:40-04:00'
describe
'559135' 'info:fdaE20100110_AAACDNfileF20100110_AABNUC' 'sip-files00035.jpg'
391a3bd4dbe7e993b73fa752abd86b85
7e061bb6ced30f4232c88f7a11e2eb230df7cdd4
'2012-05-16T12:00:43-04:00'
describe
'62166' 'info:fdaE20100110_AAACDNfileF20100110_AABNUD' 'sip-files00035.pro'
edd15ff7da3e5dd730c3144262ad9939
e1ce13399f65afe935af556a24401846983fef03
'2012-05-16T12:01:11-04:00'
describe
'178859' 'info:fdaE20100110_AAACDNfileF20100110_AABNUE' 'sip-files00035.QC.jpg'
9b64927b59f1f05cc97622467932a534
cb137f537c74eeaf9c3f2074c699e6ee561a1b18
'2012-05-16T12:03:47-04:00'
describe
'3749866' 'info:fdaE20100110_AAACDNfileF20100110_AABNUF' 'sip-files00035.tif'
fa3421fed03b27951851b94cd2a103b8
a14964b21c755e607270ab14027f90255a9958c1
'2012-05-16T11:58:06-04:00'
describe
'2481' 'info:fdaE20100110_AAACDNfileF20100110_AABNUG' 'sip-files00035.txt'
edf18108b07f3a18982c51b3de5fcbc4
b8bf813dfb9ea4c5769b5a50874a9290a3a4e822
'2012-05-16T12:06:56-04:00'
describe
'47961' 'info:fdaE20100110_AAACDNfileF20100110_AABNUH' 'sip-files00035thm.jpg'
78ea7bf93074be88ceaa47499ac7221f
22e9d7a674473f791d5d43eec0d20814567f24c5
describe
'483324' 'info:fdaE20100110_AAACDNfileF20100110_AABNUI' 'sip-files00036.jp2'
426c3625f27c6df3cb4d6242ecfbeb96
ca496a50133a04a6d8151c62df516d6587082e76
'2012-05-16T12:05:57-04:00'
describe
'491330' 'info:fdaE20100110_AAACDNfileF20100110_AABNUJ' 'sip-files00036.jpg'
47befa972a0686537024e45b9ca53a6d
92ba9936dd513fe2e1294f05e9ee44519cd6bb80
'2012-05-16T12:03:15-04:00'
describe
'58175' 'info:fdaE20100110_AAACDNfileF20100110_AABNUK' 'sip-files00036.pro'
1f1d70f6e39580b674796c9c1c6d8955
1dc744405076d3a3e53a4ada246f5fb9a6ae1dd1
describe
'153588' 'info:fdaE20100110_AAACDNfileF20100110_AABNUL' 'sip-files00036.QC.jpg'
9049a33f179d61ea82b23a8323b3c7d2
763a88db678e1438680d802a0946c3a883e2d6ec
'2012-05-16T12:07:13-04:00'
describe
'3869126' 'info:fdaE20100110_AAACDNfileF20100110_AABNUM' 'sip-files00036.tif'
39ff2201768a9479ecd8c43a4a8457f2
8c3675fcb89bd67910a1bb09c2458ca4e590761e
describe
'2613' 'info:fdaE20100110_AAACDNfileF20100110_AABNUN' 'sip-files00036.txt'
508458171402fc9930dc926ac4f15ca3
5a1623e7da726ce018ee1948d3fe1715d4da4390
'2012-05-16T11:57:14-04:00'
describe
'41856' 'info:fdaE20100110_AAACDNfileF20100110_AABNUO' 'sip-files00036thm.jpg'
0d6e896459dba79ed12eab61b4037e0b
7d09a6b8f05651cee028acbf6269453d3296572d
describe
'464918' 'info:fdaE20100110_AAACDNfileF20100110_AABNUP' 'sip-files00037.jp2'
12d8ccb9f3edc7bffa2e7b720cce519c
2f914431ce379230698266259f4ddfdf18857087
'2012-05-16T11:56:37-04:00'
describe
'550465' 'info:fdaE20100110_AAACDNfileF20100110_AABNUQ' 'sip-files00037.jpg'
9e05a77bd00ac4778156699413dba4d2
22a9884ff57cd0ac6f92986675bceb95f2840999
'2012-05-16T11:59:42-04:00'
describe
'40876' 'info:fdaE20100110_AAACDNfileF20100110_AABNUR' 'sip-files00037.pro'
8c3bdf2f546f75dfeae27c70cf9766fa
350f8153e881e7c7dc45c9f026c2d876252343c7
'2012-05-16T12:07:08-04:00'
describe
'168697' 'info:fdaE20100110_AAACDNfileF20100110_AABNUS' 'sip-files00037.QC.jpg'
630ecfd208bb74bcbf4bffb7a7a4ea9c
a1902c7dc48a99c708cb10d6e64c5cc0f18d6d71
'2012-05-16T11:57:48-04:00'
describe
'3722738' 'info:fdaE20100110_AAACDNfileF20100110_AABNUT' 'sip-files00037.tif'
91cc8afd72e01cd2ad679d049135aba5
97645715812643f55ee71a0ffbd95ae84fc8f01e
'2012-05-16T11:58:47-04:00'
describe
'1657' 'info:fdaE20100110_AAACDNfileF20100110_AABNUU' 'sip-files00037.txt'
d23bc0dc577c72d374fcbc0bfe594304
4226cce2b157c60cffb6d44c641a85eb4ab037da
describe
'46933' 'info:fdaE20100110_AAACDNfileF20100110_AABNUV' 'sip-files00037thm.jpg'
0db7648d997187b4698ba35bb0e935c0
a5abc4ab85201c2142e39a6fd6e09690265e3d5d
'2012-05-16T12:05:04-04:00'
describe
'470096' 'info:fdaE20100110_AAACDNfileF20100110_AABNUW' 'sip-files00038.jp2'
a88c13f9cd06fa08b06748be7e69072c
8214a73d27c97ca0437435ad6e357193f3718e7f
'2012-05-16T12:04:25-04:00'
describe
'574890' 'info:fdaE20100110_AAACDNfileF20100110_AABNUX' 'sip-files00038.jpg'
88bb48a73a5fb68e13abf7f0d906ffcb
660ee806da5b0a27aaf14193fbc0afd03670bf3d
'2012-05-16T12:03:03-04:00'
describe
'67401' 'info:fdaE20100110_AAACDNfileF20100110_AABNUY' 'sip-files00038.pro'
ddaffa00342adeecbdee4c08c7ab3b56
03f376603f307b4644ff21b8ef0b6b2d74ba3ed6
'2012-05-16T11:57:19-04:00'
describe
'179140' 'info:fdaE20100110_AAACDNfileF20100110_AABNUZ' 'sip-files00038.QC.jpg'
d856128a91df731225f009ffd6032b8d
af543e446ed2be025c3d48bebe2a39c14d2d6a58
'2012-05-16T11:59:01-04:00'
describe
'3763330' 'info:fdaE20100110_AAACDNfileF20100110_AABNVA' 'sip-files00038.tif'
189898452ab2a4301f1712974e5dd0f2
72ab5ebe74f3a05f7eab12372e65e333ff2d2749
'2012-05-16T11:56:51-04:00'
describe
'2710' 'info:fdaE20100110_AAACDNfileF20100110_AABNVB' 'sip-files00038.txt'
18238e725af3246dc6b2d48b74263d97
bb452ebaf8493f23af90d7fb3148f30a56ff35ff
describe
'47959' 'info:fdaE20100110_AAACDNfileF20100110_AABNVC' 'sip-files00038thm.jpg'
d46308c600f63f17d48ff1c583f4adf3
38f7dab022ec2ed4eb1308f5e047cdce439369dd
'2012-05-16T11:56:29-04:00'
describe
'473692' 'info:fdaE20100110_AAACDNfileF20100110_AABNVD' 'sip-files00039.jp2'
83528919adf2a7709d4066a4a613d7f8
29445be6f05b955c29714342af3288cccc8c559a
'2012-05-16T12:05:43-04:00'
describe
'547866' 'info:fdaE20100110_AAACDNfileF20100110_AABNVE' 'sip-files00039.jpg'
c8aad10e80a9337c96e2f283e95f143e
42043c0f11926fd74cda77d3ee4e7ab9bf0423f8
'2012-05-16T12:06:58-04:00'
describe
'36795' 'info:fdaE20100110_AAACDNfileF20100110_AABNVF' 'sip-files00039.pro'
817b9de2135b3661f5fe63aec568ff5f
907c1d45249850091a45f75505d921733fc97bc4
describe
'167848' 'info:fdaE20100110_AAACDNfileF20100110_AABNVG' 'sip-files00039.QC.jpg'
792b11d7767573f0c693b73d27d55d36
6afc06a8b0849e2d61d840dcaad7b40ecb70d5c7
'2012-05-16T11:59:36-04:00'
describe
'3792706' 'info:fdaE20100110_AAACDNfileF20100110_AABNVH' 'sip-files00039.tif'
0545485cdb6834d807f91f3ead04ee69
ebb7bb53d95c3f88181848d6220264d88112ac88
'2012-05-16T11:58:17-04:00'
describe
'1464' 'info:fdaE20100110_AAACDNfileF20100110_AABNVI' 'sip-files00039.txt'
f183bfde8facd3644a8201ba7c91b177
840c8d11996c05e36ed35b7a55a95f6d7072c5cc
'2012-05-16T12:04:46-04:00'
describe
'44053' 'info:fdaE20100110_AAACDNfileF20100110_AABNVJ' 'sip-files00039thm.jpg'
ae2b0f06335c691e3669872701d666a6
bf6b0c97ddb423af8cfedf0aece1be4fa11d42e1
'2012-05-16T12:02:52-04:00'
describe
'480192' 'info:fdaE20100110_AAACDNfileF20100110_AABNVK' 'sip-files00040.jp2'
61ffb5360ecda7e48cf0e0ab514f2bec
d40a2f1f327dfcdbd50f9a88d2786e8d4603637f
'2012-05-16T11:58:22-04:00'
describe
'534398' 'info:fdaE20100110_AAACDNfileF20100110_AABNVL' 'sip-files00040.jpg'
1b02d0222fa3d572b343516787d682f4
ad4ab002bc3b801fd926b4a684fb1ac6cd501996
'2012-05-16T12:03:06-04:00'
describe
'57413' 'info:fdaE20100110_AAACDNfileF20100110_AABNVM' 'sip-files00040.pro'
7ff1bd28e864dd1124a8b336c4539ffe
9ba93d8ea68f8cabc8e887804108d8385dae8b95
'2012-05-16T11:58:36-04:00'
describe
'170170' 'info:fdaE20100110_AAACDNfileF20100110_AABNVN' 'sip-files00040.QC.jpg'
3022d33a1ef7bd9dbcbb5faec23165db
1ff463f7c1b773358e1b6aeebaa4829c9e85b855
describe
'3844114' 'info:fdaE20100110_AAACDNfileF20100110_AABNVO' 'sip-files00040.tif'
37aa245f560a704328f4f8994d3002b5
03a893b0b7d01a37d200c527e858a3de36368441
'2012-05-16T11:56:24-04:00'
describe
'2280' 'info:fdaE20100110_AAACDNfileF20100110_AABNVP' 'sip-files00040.txt'
23879bc6dcda0ff3f83f4f294191d8a8
4b2e119968a85322ea0ea300870559b5ab864048
'2012-05-16T12:02:36-04:00'
describe
'45184' 'info:fdaE20100110_AAACDNfileF20100110_AABNVQ' 'sip-files00040thm.jpg'
3167ba49a89efd2ebec2b6b7b4fc79f1
23542352af0dd900aa6567fc14c0329cd72c07ac
describe
'482257' 'info:fdaE20100110_AAACDNfileF20100110_AABNVR' 'sip-files00041.jp2'
ff2d356ad31f9545d10a20b35b6753de
a524bb5f2a1fb0555d145657898c0e93a030f76b
describe
'504837' 'info:fdaE20100110_AAACDNfileF20100110_AABNVS' 'sip-files00041.jpg'
458852a961d09834da61258c7d35fd4a
cbd2cab6bfdddb795a89ed5a5631ee27083abeff
describe
'64806' 'info:fdaE20100110_AAACDNfileF20100110_AABNVT' 'sip-files00041.pro'
7ee3ffb96770bd8adde932f3b6e6f589
bc84b8fd739ea5694e3593af095c6042bce9e61a
'2012-05-16T12:06:45-04:00'
describe
'159729' 'info:fdaE20100110_AAACDNfileF20100110_AABNVU' 'sip-files00041.QC.jpg'
372e70875de9fe5122bab3514113f751
90ee88d20b6508fda533d40544189e1eddaef94d
'2012-05-16T12:07:17-04:00'
describe
'3860498' 'info:fdaE20100110_AAACDNfileF20100110_AABNVV' 'sip-files00041.tif'
6a80ff6ce6226177dcd1c11f3fbf25e6
9fc2fb7a1510d795edc66fc6f1db727a063ec5c7
describe
'2869' 'info:fdaE20100110_AAACDNfileF20100110_AABNVW' 'sip-files00041.txt'
4ab757682d9ae926ea99e38ece299427
2acb93f4c9ed58e22efd8b8fadd5c3911007582c
describe
'42903' 'info:fdaE20100110_AAACDNfileF20100110_AABNVX' 'sip-files00041thm.jpg'
1cdb0be7740985ebe205ee4578129ed7
75f9da72c2ecaba971dc1e6fed58359a45527b68
'2012-05-16T11:59:30-04:00'
describe
'475191' 'info:fdaE20100110_AAACDNfileF20100110_AABNVY' 'sip-files00042.jp2'
0e76f662007e49d38d6049d63dd41f47
8224c06501d23bc35c7f3db9957bbe171854bb28
'2012-05-16T11:59:15-04:00'
describe
'557424' 'info:fdaE20100110_AAACDNfileF20100110_AABNVZ' 'sip-files00042.jpg'
6003255d16581663a4ccb64d026e3027
f588d2a5a918e6a8deeeb2a858a5e487372aa1f6
describe
'62646' 'info:fdaE20100110_AAACDNfileF20100110_AABNWA' 'sip-files00042.pro'
0bf81f4bde7da1814c508b919ff68427
c20e4330114eb3e5403bcd6bdba0a85768eee762
'2012-05-16T12:01:57-04:00'
describe
'177007' 'info:fdaE20100110_AAACDNfileF20100110_AABNWB' 'sip-files00042.QC.jpg'
dfbeeb2ae27fcc057480ecd75297b5b7
275c2bbe6cbbc9cd9797bd4679998cc8c361435b
describe
'3803946' 'info:fdaE20100110_AAACDNfileF20100110_AABNWC' 'sip-files00042.tif'
f31775eff1c885742653d126f9bfbc44
ab54f61974fd7e111752e09646d37117dbbcac83
'2012-05-16T12:00:06-04:00'
describe
'2502' 'info:fdaE20100110_AAACDNfileF20100110_AABNWD' 'sip-files00042.txt'
c6c9ffe857ae1a0dd81240be2392e241
1f0e23e40ee7c23dc535ddc4565da2dc814b882a
'2012-05-16T11:58:38-04:00'
describe
'47090' 'info:fdaE20100110_AAACDNfileF20100110_AABNWE' 'sip-files00042thm.jpg'
16482ac1369210d2e169f298ede26147
61d07e4041ef7bd0d1b8ce9eb50aa20bb41b7c33
describe
'467371' 'info:fdaE20100110_AAACDNfileF20100110_AABNWF' 'sip-files00043.jp2'
7f5950f21a43fc8f81d81cedb80f22f4
d383b277a054b505a2f1e837f4a07a10d5017eef
'2012-05-16T12:01:31-04:00'
describe
'595908' 'info:fdaE20100110_AAACDNfileF20100110_AABNWG' 'sip-files00043.jpg'
82fbe265675883bc2f47740942a439d0
40742410150693cef7189d5195cc0856cfd5b15d
'2012-05-16T11:59:19-04:00'
describe
'70472' 'info:fdaE20100110_AAACDNfileF20100110_AABNWH' 'sip-files00043.pro'
29a07e89d97c83894fae8a586abd4dcc
ad2949c93f4ce72d6ec5fdcd4fce1c71adc2ca50
'2012-05-16T12:07:19-04:00'
describe
'191048' 'info:fdaE20100110_AAACDNfileF20100110_AABNWI' 'sip-files00043.QC.jpg'
43bca59bcd366938509f1be2554754ba
5a42da425f060a9a7b9302152ad267d2d995322a
describe
'3741274' 'info:fdaE20100110_AAACDNfileF20100110_AABNWJ' 'sip-files00043.tif'
45eeabc73cdd564a65e4f81615fb189e
d1ccac4f908826a402386cac48454e6845ce0267
describe
'2777' 'info:fdaE20100110_AAACDNfileF20100110_AABNWK' 'sip-files00043.txt'
9914e6a15e219ef26e8b91613d91520d
4efa45d4398b0c72af519ca194b496a12e505488
'2012-05-16T11:58:32-04:00'
describe
'49984' 'info:fdaE20100110_AAACDNfileF20100110_AABNWL' 'sip-files00043thm.jpg'
be8a5b974b124388980ec37f6de49de4
d51e2e313f35606959151cd99399a710f2db10b5
'2012-05-16T12:06:22-04:00'
describe
'479199' 'info:fdaE20100110_AAACDNfileF20100110_AABNWM' 'sip-files00044.jp2'
ef4bc295d5b52e32a49d6b140014e7c9
f02e28afa9b8f3004fc2c2dc3d5fc628be2e08d4
'2012-05-16T12:04:37-04:00'
describe
'539172' 'info:fdaE20100110_AAACDNfileF20100110_AABNWN' 'sip-files00044.jpg'
06fe4546820d32273c912ad2d55a8978
ef82328c1f92a4c2f02c9da743ccd2917854ec29
'2012-05-16T12:02:09-04:00'
describe
'56803' 'info:fdaE20100110_AAACDNfileF20100110_AABNWO' 'sip-files00044.pro'
ce28e582f4d8085de79f274d22e93126
b66996dcef79ee2112b5380bf3a6857e49ee7845
'2012-05-16T12:04:43-04:00'
describe
'168773' 'info:fdaE20100110_AAACDNfileF20100110_AABNWP' 'sip-files00044.QC.jpg'
61fc3df31600233504e70e03084c43a9
a5867dfa2cf9e70987b838b1ab877e5b1fe64b76
'2012-05-16T12:07:14-04:00'
describe
'3836018' 'info:fdaE20100110_AAACDNfileF20100110_AABNWQ' 'sip-files00044.tif'
4ca06a30477561f8611b7272a2ba9db4
f2575565cd641ae23bac949ffbd6bdf4daf571f1
'2012-05-16T12:07:16-04:00'
describe
'2327' 'info:fdaE20100110_AAACDNfileF20100110_AABNWR' 'sip-files00044.txt'
b2d75debd1cb411b7ddb870f58decd7c
adeeed8425858efec96dd2caad88fce718b22222
'2012-05-16T12:01:55-04:00'
describe
'44230' 'info:fdaE20100110_AAACDNfileF20100110_AABNWS' 'sip-files00044thm.jpg'
6cacd3e716772212c5417164cb222323
292f928355f52e6c42bd5c3d45ec4e645c46593a
'2012-05-16T11:57:38-04:00'
describe
'475308' 'info:fdaE20100110_AAACDNfileF20100110_AABNWT' 'sip-files00045.jp2'
7fc10703395309c153b5aff6eec61365
7ab6e1ec21dbe610c5647ef53b096362bda69278
'2012-05-16T12:04:38-04:00'
describe
'549793' 'info:fdaE20100110_AAACDNfileF20100110_AABNWU' 'sip-files00045.jpg'
911c7cb628cef0c27b953a361df3580e
ec3f4bd287b88b39dac4815010fd68126e69ceaa
'2012-05-16T12:04:11-04:00'
describe
'61226' 'info:fdaE20100110_AAACDNfileF20100110_AABNWV' 'sip-files00045.pro'
187d1b779c44662448561849638a5612
0b3aeb841ad954aa3d5d8276590cba1e7aa9cea1
describe
'177774' 'info:fdaE20100110_AAACDNfileF20100110_AABNWW' 'sip-files00045.QC.jpg'
30acd440ee91e1259e8b3b7825c39794
8b0b68822ca73a93dbfef38cc223e20ff8068b5a
'2012-05-16T11:57:31-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABNWX' 'sip-files00045.tif'
540aeb72c3f2fbcb3c47c93d1466e1bc
3adb5cc6601dd43176b426ff29532fcbd2fa62c9
'2012-05-16T12:01:04-04:00'
describe
'2437' 'info:fdaE20100110_AAACDNfileF20100110_AABNWY' 'sip-files00045.txt'
3750a7792cb065f99befcbd354156088
ef9c9eeb54e15b559b4d71fc6d92598537b52c11
'2012-05-16T12:04:23-04:00'
describe
'48802' 'info:fdaE20100110_AAACDNfileF20100110_AABNWZ' 'sip-files00045thm.jpg'
2ccc5e635bf160c244686526f4b23c6b
f604f1734b2bfdc5d1b4dbc10fb3f5b8ad3f1f0a
'2012-05-16T11:56:16-04:00'
describe
'472572' 'info:fdaE20100110_AAACDNfileF20100110_AABNXA' 'sip-files00046.jp2'
6849e92babdf9994e5921e333f7a8411
77329ea9693ad032575d049b45d8b9045f1cdb6a
'2012-05-16T12:07:18-04:00'
describe
'172413' 'info:fdaE20100110_AAACDNfileF20100110_AABNXB' 'sip-files00046.jpg'
6a5838671b19199fe3665088e0c73eba
8f145c464bbc5f903774699266b81864639d20cc
describe
'10673' 'info:fdaE20100110_AAACDNfileF20100110_AABNXC' 'sip-files00046.pro'
4c2770dd381d02f93b5ef070f790d175
fdd26fac413ca475828e380380dd68d872029d9d
describe
'59912' 'info:fdaE20100110_AAACDNfileF20100110_AABNXD' 'sip-files00046.QC.jpg'
157d803d391848267a5b7453a520524c
9fff29300a5fac996f7201156be871bb259768da
'2012-05-16T12:01:26-04:00'
describe
'3807688' 'info:fdaE20100110_AAACDNfileF20100110_AABNXE' 'sip-files00046.tif'
344be2bf07322ac6baece3658d8390b3
8076259dd0fbebb5db8d06718ac0a504ff0ce9a5
'2012-05-16T12:02:26-04:00'
describe
'592' 'info:fdaE20100110_AAACDNfileF20100110_AABNXF' 'sip-files00046.txt'
fafff8d9706400b5f30794b0318197ce
d66914e0c593fa08a792bf7ca4e4b6142c5b0146
'2012-05-16T11:57:09-04:00'
describe
WARNING CODE 'Daitss::Anomaly' Invalid character
'26143' 'info:fdaE20100110_AAACDNfileF20100110_AABNXG' 'sip-files00046thm.jpg'
d2e599c5fc9f0c0a721bc38a4019ca37
317722dba150e82379f3a24cb7247165adcb5192
describe
'477122' 'info:fdaE20100110_AAACDNfileF20100110_AABNXH' 'sip-files00047.jp2'
09879e631473b72593e2626352b71cf3
51042776ec9224082a29a5ecd928aa99c1c7d55d
'2012-05-16T12:03:32-04:00'
describe
'494178' 'info:fdaE20100110_AAACDNfileF20100110_AABNXI' 'sip-files00047.jpg'
ba85dca880055483c78ebf66c1a1c973
691607751004566fb103ebda583739bfab366f18
'2012-05-16T12:05:08-04:00'
describe
'37048' 'info:fdaE20100110_AAACDNfileF20100110_AABNXJ' 'sip-files00047.pro'
12fcde1d09ae9a49b06f1bc7d02b0d81
b7737707caccf8cc6d97c333c67fd1084cddc3fe
describe
'153638' 'info:fdaE20100110_AAACDNfileF20100110_AABNXK' 'sip-files00047.QC.jpg'
e2b8e5c4f547a84bcb28d296b290a80e
09f9673d0ba554f50e6e6704208c28f1996d95e0
describe
'3819994' 'info:fdaE20100110_AAACDNfileF20100110_AABNXL' 'sip-files00047.tif'
e0bd7d0d3c260a4a54491ad953c5f57d
196d9bd1bbfca6fd57dd4be2b52d055782f45ddf
describe
'1518' 'info:fdaE20100110_AAACDNfileF20100110_AABNXM' 'sip-files00047.txt'
02800268e32d3e25adb8e6219d201f52
dc602efd627ed130aed1787629b806a197698974
'2012-05-16T12:01:56-04:00'
describe
'42233' 'info:fdaE20100110_AAACDNfileF20100110_AABNXN' 'sip-files00047thm.jpg'
5f9c82c46576a4784cc5826fbcdd1dc0
36215ceef777b1745319e2b0088a000a40298679
'2012-05-16T12:03:55-04:00'
describe
'477028' 'info:fdaE20100110_AAACDNfileF20100110_AABNXO' 'sip-files00048.jp2'
96e78e2d51e47ce574c753dc3ef1470c
b863fd5d456f50d36a6151b24dd55d252dd6c2e4
'2012-05-16T11:59:32-04:00'
describe
'487973' 'info:fdaE20100110_AAACDNfileF20100110_AABNXP' 'sip-files00048.jpg'
e5ad37e5e82f108d6d65ec775d4123c0
8152df69282d214ae8166beb1877864febbe1275
describe
'43453' 'info:fdaE20100110_AAACDNfileF20100110_AABNXQ' 'sip-files00048.pro'
f41436a1bf2419e63dd9ea5e87c81ef7
b9fec5829f0a601562d5f47eca698db27fddb534
'2012-05-16T12:04:32-04:00'
describe
'146855' 'info:fdaE20100110_AAACDNfileF20100110_AABNXR' 'sip-files00048.QC.jpg'
ae020bef94c4314d4835df55029cc1d1
a1bf39829d822e1be79dbc515e0f39098e8e0fdb
describe
'3818782' 'info:fdaE20100110_AAACDNfileF20100110_AABNXS' 'sip-files00048.tif'
e9350afa258e4b498aa448a015cb104f
7fa015bcbfa919f202f0ebd3f4eba31a0886be89
'2012-05-16T12:01:01-04:00'
describe
'1888' 'info:fdaE20100110_AAACDNfileF20100110_AABNXT' 'sip-files00048.txt'
f7a583d1746fc8480bd3a979e57577de
9c8dbb0d60e54559a444651c4de1c7accb932c16
'2012-05-16T11:57:29-04:00'
describe
'39672' 'info:fdaE20100110_AAACDNfileF20100110_AABNXU' 'sip-files00048thm.jpg'
1e38c7aaa945e5e4b692bbb5bac1c256
b6bea3bdaff0ced1b05e2748bd94177fe6aa8bc1
'2012-05-16T12:05:09-04:00'
describe
'470019' 'info:fdaE20100110_AAACDNfileF20100110_AABNXV' 'sip-files00049.jp2'
b01efc8e6136f7c67cbf480be4d69ef0
8e664c0e7f3faf2f221b17b8b5dd99870156b07d
'2012-05-16T12:00:00-04:00'
describe
'576702' 'info:fdaE20100110_AAACDNfileF20100110_AABNXW' 'sip-files00049.jpg'
4f7fc2d9a218be8df8049b9a5a926637
c4b6c9d7878ad41c3393871af4386217ef112d3e
'2012-05-16T12:06:55-04:00'
describe
'64146' 'info:fdaE20100110_AAACDNfileF20100110_AABNXX' 'sip-files00049.pro'
975d4a9b31c3af0fca5fe15d9218cd07
f259d0172e7ca72333a1b6cd9d7e40448511736e
describe
'186205' 'info:fdaE20100110_AAACDNfileF20100110_AABNXY' 'sip-files00049.QC.jpg'
a1625b7bb241ab4582db77b343eb6d09
a786656fc1435a26d81868746ecbc0180c473978
describe
'3763138' 'info:fdaE20100110_AAACDNfileF20100110_AABNXZ' 'sip-files00049.tif'
b45d77b198235536161a7fd6c19c5e63
6bf7e619f2c20299d37d3aacf6820b7cf4ba226d
'2012-05-16T12:04:57-04:00'
describe
'2556' 'info:fdaE20100110_AAACDNfileF20100110_AABNYA' 'sip-files00049.txt'
3b09ad320623008a594350b42ff083a7
e441b3582811f6134a51ef21245595695b5afe8f
describe
'49689' 'info:fdaE20100110_AAACDNfileF20100110_AABNYB' 'sip-files00049thm.jpg'
b44cb545aaa5bd8fa4cb5dfdf75447bb
19c1996ae593e4ba5f2709c29fa7ff3118f17485
'2012-05-16T12:03:54-04:00'
describe
'475198' 'info:fdaE20100110_AAACDNfileF20100110_AABNYC' 'sip-files00050.jp2'
01ef6782cc243777016ebe1d1497b20b
c51abc74658b239b7b8767fe04b0c422bf41efc6
'2012-05-16T12:06:59-04:00'
describe
'494625' 'info:fdaE20100110_AAACDNfileF20100110_AABNYD' 'sip-files00050.jpg'
28e53b4149d1fe87c57ae613a857938a
aa270a969c42d90e39773ca16399f1dcc83cbc08
describe
'39019' 'info:fdaE20100110_AAACDNfileF20100110_AABNYE' 'sip-files00050.pro'
e9bfd3523f521e13835097064fa69280
e5b20963791b123b4c552e1685dd11419e29bc1c
describe
'155299' 'info:fdaE20100110_AAACDNfileF20100110_AABNYF' 'sip-files00050.QC.jpg'
bb66c8de8ca09375538f7d7fe527f32a
711d248cbb52c6f9a0bbcfcb2e3cdc0c668a9eb8
'2012-05-16T12:06:33-04:00'
describe
'3803918' 'info:fdaE20100110_AAACDNfileF20100110_AABNYG' 'sip-files00050.tif'
8f7368ef698d78c990c2e2d76c343ec4
43492db662e6404200642241a088ba5fcab5f647
'2012-05-16T12:01:12-04:00'
describe
'1550' 'info:fdaE20100110_AAACDNfileF20100110_AABNYH' 'sip-files00050.txt'
248e3f96643ae098de7507be0762cf62
fb3289c55744b6ba14c8825689e5c4d5a950a3c5
'2012-05-16T12:07:15-04:00'
describe
Invalid character
'41532' 'info:fdaE20100110_AAACDNfileF20100110_AABNYI' 'sip-files00050thm.jpg'
ed12c7103a140021a3783f6ed2610370
387401189eef56304011e79921377c1bf4d947a8
'2012-05-16T12:04:21-04:00'
describe
'473468' 'info:fdaE20100110_AAACDNfileF20100110_AABNYJ' 'sip-files00051.jp2'
5e29a40fff587c4c7ff89347b81c5e22
2e021f0f39edb6f7820639b30be1d60249972675
describe
'564853' 'info:fdaE20100110_AAACDNfileF20100110_AABNYK' 'sip-files00051.jpg'
1dcadf5bc629a6a8ed1b68c5fde800c4
c5453c63e30ca3d9b0d6d6c9fce786e17eb7d0b1
'2012-05-16T12:05:27-04:00'
describe
'61410' 'info:fdaE20100110_AAACDNfileF20100110_AABNYL' 'sip-files00051.pro'
cfa4be7cc42f052249bf869037c669ce
e3e027906adcde5eac865674386afde78ad0984f
'2012-05-16T11:57:40-04:00'
describe
'179725' 'info:fdaE20100110_AAACDNfileF20100110_AABNYM' 'sip-files00051.QC.jpg'
40aeedcd321621a2ac25192096200d33
90bfbef4b5c8553698d3a2e30c4c3230a0e3251b
'2012-05-16T11:58:05-04:00'
describe
'3790330' 'info:fdaE20100110_AAACDNfileF20100110_AABNYN' 'sip-files00051.tif'
0ca8bc0b16bd6e4311a42180e1da70fb
6c75c817a5961bb836b33dd239df5ab4df76e0f1
'2012-05-16T12:03:25-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABNYO' 'sip-files00051.txt'
ffe9e473741beae054df49580c3db2b4
b791c1bde66b32594a4f35a98d27cc763964165f
describe
'48844' 'info:fdaE20100110_AAACDNfileF20100110_AABNYP' 'sip-files00051thm.jpg'
fceb61c9a9942ff1945c477c635b9c7a
99b0bf3ea49dda6c42c684b2e361d1591561f855
'2012-05-16T11:57:16-04:00'
describe
'471709' 'info:fdaE20100110_AAACDNfileF20100110_AABNYQ' 'sip-files00052.jp2'
0b6a4d0831a4237965a7f850623821d5
e632800c42deb53b4504857b7535dd2637e29fcc
describe
'499885' 'info:fdaE20100110_AAACDNfileF20100110_AABNYR' 'sip-files00052.jpg'
8810a24fc0a3beb92bcc4d74f8b16214
861defd0d6a114c7bc1903fe69a6baa9f6e8cc37
'2012-05-16T11:56:53-04:00'
describe
'8342' 'info:fdaE20100110_AAACDNfileF20100110_AABNYS' 'sip-files00052.pro'
baa306cb783ea96e5d8e1c43511fb95c
5cea404f151f9cbed5a7637d44a28aeb0ba024c6
'2012-05-16T11:58:43-04:00'
describe
'142320' 'info:fdaE20100110_AAACDNfileF20100110_AABNYT' 'sip-files00052.QC.jpg'
636de048c9252450aee8899ad8b96fe2
7bbfb0b7ca31832c551721a07ec6115de5ae150d
'2012-05-16T12:02:30-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABNYU' 'sip-files00052.tif'
766a775098907cec1da9db442064a713
b370fb9e85b900679a2f3c4a1568cffb7afda42c
'2012-05-16T12:03:05-04:00'
describe
'407' 'info:fdaE20100110_AAACDNfileF20100110_AABNYV' 'sip-files00052.txt'
f31acc0cdcf3334bf391da94c1038b1e
e8825a76263c0339a860d220e9a5ace71f9b2b9e
'2012-05-16T12:06:51-04:00'
describe
'39178' 'info:fdaE20100110_AAACDNfileF20100110_AABNYW' 'sip-files00052thm.jpg'
2fadc908bb26ed00a3a36b23e7132193
45a695f68e9e62e66330e0f3dd3ffbd51ed53a75
describe
'467121' 'info:fdaE20100110_AAACDNfileF20100110_AABNYX' 'sip-files00053.jp2'
f816ae25e95e14507e409b2f9fd81a11
0267bf339a3a797f746b31dc038042b4477c079e
describe
'459333' 'info:fdaE20100110_AAACDNfileF20100110_AABNYY' 'sip-files00053.jpg'
24fa46d26768e9ef5aa167a3eff4fff7
ae07ecb12acaf877d1bffd1ae241f346497be865
'2012-05-16T11:59:34-04:00'
describe
'40901' 'info:fdaE20100110_AAACDNfileF20100110_AABNYZ' 'sip-files00053.pro'
edf8485fe137eeec9aa448df83dc5675
73958d6a6548aa7ff4d48616b620de8fca976940
'2012-05-16T12:01:40-04:00'
describe
'144593' 'info:fdaE20100110_AAACDNfileF20100110_AABNZA' 'sip-files00053.QC.jpg'
a31723036e9f6645670858f3efc6040a
45c89d2f2bf9aebc6ba7bf80130c6eac7e363fb3
'2012-05-16T11:58:24-04:00'
describe
'3739658' 'info:fdaE20100110_AAACDNfileF20100110_AABNZB' 'sip-files00053.tif'
a16b09e4fb6474aad6087afc1e17cd3c
c0b8c908867026763a95c221fc07664225d4f038
'2012-05-16T11:57:15-04:00'
describe
'1619' 'info:fdaE20100110_AAACDNfileF20100110_AABNZC' 'sip-files00053.txt'
bd89350e8af153ef9fbf6265d0081b52
0898b85f62f1c301ff855fbe86c3ee3713586a81
'2012-05-16T12:00:41-04:00'
describe
'37980' 'info:fdaE20100110_AAACDNfileF20100110_AABNZD' 'sip-files00053thm.jpg'
a74d2bd4d71d13c3ae6ecfe64d9a4ba6
df5c1b4e18fc2b2b7655bac258f2d158e97fa350
'2012-05-16T12:00:47-04:00'
describe
'475454' 'info:fdaE20100110_AAACDNfileF20100110_AABNZE' 'sip-files00054.jp2'
de97e8ea85efaddd6a487b73a41a1101
2a8d50e369a34849f92fda0bedb8c43934b1c1ad
describe
'184109' 'info:fdaE20100110_AAACDNfileF20100110_AABNZF' 'sip-files00054.jpg'
abaff419676b891b9d2f87163b689096
89d35a0325f1b4fc95f0e95ff954d1924228df79
describe
'10298' 'info:fdaE20100110_AAACDNfileF20100110_AABNZG' 'sip-files00054.pro'
6357f2247803e8e13327c8dda9be3b4d
dcbbc0fa585f3734356bb3a0b37ddd426a652049
'2012-05-16T12:05:11-04:00'
describe
'64549' 'info:fdaE20100110_AAACDNfileF20100110_AABNZH' 'sip-files00054.QC.jpg'
0949864b64bb409d90a3bea45bb20e20
a2e766bea8c9ba7afdc663655f56f5916a92b28f
describe
'4148818' 'info:fdaE20100110_AAACDNfileF20100110_AABNZI' 'sip-files00054.tif'
dc38a000746d8ef004b2605aa2dc1263
ec88d2783c17e07a29143ca8ef8330a4adf1ebea
'2012-05-16T11:59:17-04:00'
describe
'543' 'info:fdaE20100110_AAACDNfileF20100110_AABNZJ' 'sip-files00054.txt'
23541fcaca8b32cd679134fa9590e95a
2b2bb68f5802bd3d75b87e30f7026f8e12b7f4f8
'2012-05-16T11:58:58-04:00'
describe
Invalid character
'27315' 'info:fdaE20100110_AAACDNfileF20100110_AABNZK' 'sip-files00054thm.jpg'
abb57ba6ac240c19b9adc407cc3b2391
44fe0948edbb7ab368ba4f18b3dd85f437ab9042
describe
'473372' 'info:fdaE20100110_AAACDNfileF20100110_AABNZL' 'sip-files00055.jp2'
493ed5698dae45bcb388f0164b00fcb1
b930da10c101b8a2e909d588e4792cbe9d7210e9
'2012-05-16T12:05:47-04:00'
describe
'449993' 'info:fdaE20100110_AAACDNfileF20100110_AABNZM' 'sip-files00055.jpg'
ad7a9f11f844dc0518c0fcf427d70249
b096c000fc6fde56f75cb459b1d2b77793878aeb
'2012-05-16T12:03:16-04:00'
describe
'53015' 'info:fdaE20100110_AAACDNfileF20100110_AABNZN' 'sip-files00055.pro'
61c1e3050cb4f959c60be01ae956745d
02cdcc1518d691967bfe7b6f2020b520122ba54a
'2012-05-16T11:59:35-04:00'
describe
'144811' 'info:fdaE20100110_AAACDNfileF20100110_AABNZO' 'sip-files00055.QC.jpg'
0ebb2b3e0818de955c82b49dfbf7cad8
ea0cb4e824852bf348b3df33a68bdc986e720f07
'2012-05-16T12:01:44-04:00'
describe
'3790006' 'info:fdaE20100110_AAACDNfileF20100110_AABNZP' 'sip-files00055.tif'
06b0a53b0e5afcf588b0e56c298e53ae
6389ba002738b3920c230e060d7bbe66670b4b8f
'2012-05-16T11:58:34-04:00'
describe
'2542' 'info:fdaE20100110_AAACDNfileF20100110_AABNZQ' 'sip-files00055.txt'
b0db7ffded13f5c2881cb0f153fdb89d
6c8fbb4b409684da6cb93888ce0bc870bc6658d3
'2012-05-16T12:05:16-04:00'
describe
'39417' 'info:fdaE20100110_AAACDNfileF20100110_AABNZR' 'sip-files00055thm.jpg'
97ce60b7e3bc8cecf77f2acc4863cbd0
a4c3bb1dadb62d05b860587151ad52cac0ddc42e
'2012-05-16T12:04:22-04:00'
describe
'487331' 'info:fdaE20100110_AAACDNfileF20100110_AABNZS' 'sip-files00056.jp2'
34ca1d0d9a5a6b63c45360701a9ae7c7
ecaf0ae256f4d7ec6bb3ba730db29980be176640
'2012-05-16T11:56:33-04:00'
describe
'587679' 'info:fdaE20100110_AAACDNfileF20100110_AABNZT' 'sip-files00056.jpg'
b03390885a3aa611dc44e07431bcfa3f
48e58469eaa1862e5a70886eb9350672378269c9
describe
'68525' 'info:fdaE20100110_AAACDNfileF20100110_AABNZU' 'sip-files00056.pro'
08cf9f63b38d7eb832851de4aab60cc4
6b4d588204294aedac619021aa100eaeb0b94219
describe
'184930' 'info:fdaE20100110_AAACDNfileF20100110_AABNZV' 'sip-files00056.QC.jpg'
a456fcfb79051cb6f330198700fd933d
6189e379d87915208079b2d44dfa96a4aac31d87
'2012-05-16T12:02:46-04:00'
describe
'3901698' 'info:fdaE20100110_AAACDNfileF20100110_AABNZW' 'sip-files00056.tif'
4a86ea3632a2d7da5d5444b0f555dbfa
b77dc8fff13d44ce4946ada9546296a7d32814d0
'2012-05-16T12:03:28-04:00'
describe
'2702' 'info:fdaE20100110_AAACDNfileF20100110_AABNZX' 'sip-files00056.txt'
adaec480f93f91486b0c48f66716e0b0
c6c3c46b6f1ff5580a154f5cef92ec1176b826e7
'2012-05-16T12:03:42-04:00'
describe
'48510' 'info:fdaE20100110_AAACDNfileF20100110_AABNZY' 'sip-files00056thm.jpg'
744b2414fc550580e2e828ce4c16eed5
b95293425eebbe758a6466e0d9eb03d62809f1a9
'2012-05-16T12:00:32-04:00'
describe
'481570' 'info:fdaE20100110_AAACDNfileF20100110_AABNZZ' 'sip-files00057.jp2'
9257a6ac7c7c17a9882e75859b042837
c0cdaf6fcbe901a3f7876e55a42b0d744801999f
'2012-05-16T12:06:23-04:00'
describe
'549931' 'info:fdaE20100110_AAACDNfileF20100110_AABOAA' 'sip-files00057.jpg'
9b82f311dd042bfebfa9fb8b499a4aa7
cb2c27ea0a26dd333295c745521b2483f9fb38f4
'2012-05-16T11:56:25-04:00'
describe
'64277' 'info:fdaE20100110_AAACDNfileF20100110_AABOAB' 'sip-files00057.pro'
c4a4bf6ade2ba181e9a87feb80bdede6
8e5ae875a349bca17f4b1175a852b8dd0cc820d7
describe
'177059' 'info:fdaE20100110_AAACDNfileF20100110_AABOAC' 'sip-files00057.QC.jpg'
2b38f724162dab2f0d9967ed5484f0b2
9b03012e77f30bd77674ce4fcbb29dcd67e428a5
'2012-05-16T12:06:17-04:00'
describe
'3854946' 'info:fdaE20100110_AAACDNfileF20100110_AABOAD' 'sip-files00057.tif'
a7232afa82ccd9b96bff47395b6a2222
a89bc99acaba41f14b82dcab016f6ac5ca511cfb
describe
'2540' 'info:fdaE20100110_AAACDNfileF20100110_AABOAE' 'sip-files00057.txt'
0cde10e09394c931d5345609607598be
bee4dec26880c7cff92fa6c50d00cfed121a0ffb
describe
'46404' 'info:fdaE20100110_AAACDNfileF20100110_AABOAF' 'sip-files00057thm.jpg'
b8708ff6e703124be7cda325b503b6f1
d6df0ca83ec0ccf62c02e83b4d8982f7da702dff
'2012-05-16T12:06:32-04:00'
describe
'461880' 'info:fdaE20100110_AAACDNfileF20100110_AABOAG' 'sip-files00058.jp2'
a0b7ee7060d72f775524b7050aa8a1cf
10bada141bb1da6ca945f82ca37facad897453d2
'2012-05-16T12:06:49-04:00'
describe
'542643' 'info:fdaE20100110_AAACDNfileF20100110_AABOAH' 'sip-files00058.jpg'
d69a2e107f6c48cfc0fde11d6dfca537
3e03570982c6db188afb3b9775f492563e3a8ef6
'2012-05-16T12:06:27-04:00'
describe
'58203' 'info:fdaE20100110_AAACDNfileF20100110_AABOAI' 'sip-files00058.pro'
007a4dfa12b39eac743603a6acf40466
055165f7f81f76dd90f03419bc787e4274283721
'2012-05-16T12:02:21-04:00'
describe
'177374' 'info:fdaE20100110_AAACDNfileF20100110_AABOAJ' 'sip-files00058.QC.jpg'
21ed77d3cef3c1b0869945cf13257b92
61eef99b957a3193d7ac3a0ca93eb0c76b998fd0
'2012-05-16T12:02:25-04:00'
describe
'3697354' 'info:fdaE20100110_AAACDNfileF20100110_AABOAK' 'sip-files00058.tif'
74bacc9305755c4aa688ad81ae649b81
5d5b68203b4fec21cff9afff8553159f3d7a9f99
'2012-05-16T12:02:17-04:00'
describe
'2359' 'info:fdaE20100110_AAACDNfileF20100110_AABOAL' 'sip-files00058.txt'
f5fd76873743f82f8316e8e0effb713b
216b7b01768b8e31a1c5e32624bff6caf2f7c0fd
describe
'47903' 'info:fdaE20100110_AAACDNfileF20100110_AABOAM' 'sip-files00058thm.jpg'
3b5fd27142ded5ad5f7dea88b1054512
7f1a6e5e2645171238518ad25c552d990b4ef141
'2012-05-16T12:04:00-04:00'
describe
'456559' 'info:fdaE20100110_AAACDNfileF20100110_AABOAN' 'sip-files00059.jp2'
553257cef110e33f31c982bab7349ff9
9120ca4ad819e6f4663f9e82531f41419a94fcea
'2012-05-16T11:59:55-04:00'
describe
'475341' 'info:fdaE20100110_AAACDNfileF20100110_AABOAO' 'sip-filesi.jp2'
c5f5c78db02a1c8e5517ff750da71638
46f943787ac8c248085358172af6e1786ee3cbfa
'2012-05-16T12:02:54-04:00'
describe
'549251' 'info:fdaE20100110_AAACDNfileF20100110_AABOAP' 'sip-files00059.jpg'
7f4c23d251def3a2f737e505b897d802
b1f760660d1b508821063d0b954586824a507312
'2012-05-16T12:05:37-04:00'
describe
'62371' 'info:fdaE20100110_AAACDNfileF20100110_AABOAQ' 'sip-files00059.pro'
ad96544740edec17fa034da28d7b1437
90c8165451cecf78795cc88732f584a1223850fd
describe
'179155' 'info:fdaE20100110_AAACDNfileF20100110_AABOAR' 'sip-files00059.QC.jpg'
0d50e263caae605e1f5f14b93d54b4d6
034131da702fca748c0e00fd32b061a47bdb7acf
'2012-05-16T12:00:26-04:00'
describe
'3655476' 'info:fdaE20100110_AAACDNfileF20100110_AABOAS' 'sip-files00059.tif'
f9b0dde4d1fce26a473ebdc002560b49
364cc90295b1f88595c4a4168a43abcb92be8ded
'2012-05-16T12:00:03-04:00'
describe
'2477' 'info:fdaE20100110_AAACDNfileF20100110_AABOAT' 'sip-files00059.txt'
3bdeda90a4cf91571a2348927fa89804
47d3b1515311dd8605191a1137d1b315a898b167
'2012-05-16T11:58:19-04:00'
describe
'49039' 'info:fdaE20100110_AAACDNfileF20100110_AABOAU' 'sip-files00059thm.jpg'
72fd4b8f0e8f1d927e7b24717e74e44c
b667b34c82f451d930b95c9f8d32a39b896cb3bb
'2012-05-16T11:56:15-04:00'
describe
'462960' 'info:fdaE20100110_AAACDNfileF20100110_AABOAV' 'sip-files00060.jp2'
905855771588b3e453af12daf878330e
cd8cd259b35218a6e7b39da5af2eb8c4505b5fc5
'2012-05-16T12:06:25-04:00'
describe
'172222' 'info:fdaE20100110_AAACDNfileF20100110_AABOAW' 'sip-files00060.jpg'
15f3ff68720aab1bda1e07603fa84bd5
2d5f159f18a81a1e5da5d244db503e99b7817290
'2012-05-16T11:56:52-04:00'
describe
'9438' 'info:fdaE20100110_AAACDNfileF20100110_AABOAX' 'sip-files00060.pro'
b0a45b34b2f812adb282d4c8d19c9533
c959dcf1d1af5dc060353058108ce19923bac56e
'2012-05-16T12:02:06-04:00'
describe
'60847' 'info:fdaE20100110_AAACDNfileF20100110_AABOAY' 'sip-files00060.QC.jpg'
ed01128760dcb0f737d09b12031a287e
33e9961172466022ec2ffa85547f4b9c20710250
'2012-05-16T12:00:09-04:00'
describe
'3747240' 'info:fdaE20100110_AAACDNfileF20100110_AABOAZ' 'sip-files00060.tif'
cb7a72ec9f5a84a4ae023238dd293a22
72ebcd750d84ddbc439e04c3cabb795bc5bda217
'2012-05-16T11:59:18-04:00'
describe
'518' 'info:fdaE20100110_AAACDNfileF20100110_AABOBA' 'sip-files00060.txt'
28842e0fca6eaac5172e0a5be3d4caaa
396147a5308d3418ed85620887ff94074a90f659
'2012-05-16T12:03:11-04:00'
describe
'26068' 'info:fdaE20100110_AAACDNfileF20100110_AABOBB' 'sip-files00060thm.jpg'
1ebff68d43b9070a27e763eb443e40b9
8f05e346ba8cd98fb3a03741ac4dea9e65e453e9
'2012-05-16T11:56:38-04:00'
describe
'463189' 'info:fdaE20100110_AAACDNfileF20100110_AABOBC' 'sip-files00061.jp2'
1b85b25e0aa02876b4ffe7ce95b2fbf3
97bcbaacb9330a62c04ed2f9897ed35547b32901
'2012-05-16T12:01:59-04:00'
describe
'181564' 'info:fdaE20100110_AAACDNfileF20100110_AABOBD' 'sip-files00061.jpg'
72540393ee993bef4fedbad86606a4fc
fcc0b0b9d89e25e9a5b8215557af0ff8f6e6fedd
'2012-05-16T12:01:27-04:00'
describe
'18635' 'info:fdaE20100110_AAACDNfileF20100110_AABOBE' 'sip-files00061.pro'
b897fb238140eb1c812b96f74ab89adc
8b9827404a1f9a21c48acd2245a1c7a94129f43d
'2012-05-16T12:05:03-04:00'
describe
'63525' 'info:fdaE20100110_AAACDNfileF20100110_AABOBF' 'sip-files00061.QC.jpg'
eb4f4d58853801f6bab8c0204676d992
3cc47b8f375deae6c3daae84ee1f61e9dcac5504
'2012-05-16T11:58:45-04:00'
describe
'4213678' 'info:fdaE20100110_AAACDNfileF20100110_AABOBG' 'sip-files00061.tif'
c958cfa49af8ab0c0f688761bbd3d50c
6f86a004fbab479dd701483a92284af40a11d06c
describe
'1163' 'info:fdaE20100110_AAACDNfileF20100110_AABOBH' 'sip-files00061.txt'
a8489d19caf7db9a646eb4657984271e
04db0a0f6b2c3b441861ef2390529802d91cd0b0
describe
Invalid character
'27073' 'info:fdaE20100110_AAACDNfileF20100110_AABOBI' 'sip-files00061thm.jpg'
510b4dfb3031fddaa1a79fc01c6f8722
c8303928f38a22a5ad6807a0a4574d007f4e8500
describe
'459215' 'info:fdaE20100110_AAACDNfileF20100110_AABOBJ' 'sip-files00062.jp2'
264287358b45d266b870a7234b3b116c
15bb6380281dc86ad26d30e45a96197239194669
describe
'548595' 'info:fdaE20100110_AAACDNfileF20100110_AABOBK' 'sip-files00062.jpg'
cb4a039eff440a04241badb7c43eae41
44dbb8ebcd9baa45466422bc450cc75970f49b1c
'2012-05-16T12:04:09-04:00'
describe
'40169' 'info:fdaE20100110_AAACDNfileF20100110_AABOBL' 'sip-files00062.pro'
6a7e17360c885fe2aa068035fa332e4f
19e9d627970f4143df45cebb284732bb7bb0d3d4
'2012-05-16T11:56:18-04:00'
describe
'171976' 'info:fdaE20100110_AAACDNfileF20100110_AABOBM' 'sip-files00062.QC.jpg'
c6a3bc6a475984e6cfa8af9caf3a4b84
024bcbac66469a47934798362d1a43166ade4bf8
'2012-05-16T12:02:11-04:00'
describe
'3676386' 'info:fdaE20100110_AAACDNfileF20100110_AABOBN' 'sip-files00062.tif'
a5bd228421aeef1f4408167f4b29e33c
710320966357eeb410974d7981ed96f043c0c74d
'2012-05-16T12:06:31-04:00'
describe
'1638' 'info:fdaE20100110_AAACDNfileF20100110_AABOBO' 'sip-files00062.txt'
8a69a06c7382580619e4c53fb1a1b39c
9f0e4bd52c95a28e1822966aa99ed0eb88b6bd70
'2012-05-16T12:01:50-04:00'
describe
'46409' 'info:fdaE20100110_AAACDNfileF20100110_AABOBP' 'sip-files00062thm.jpg'
40431114be93f001e124fea6f3ec30a4
48638cf65a9da2b9585ee72558a04d16b3b31abd
'2012-05-16T11:59:56-04:00'
describe
'462906' 'info:fdaE20100110_AAACDNfileF20100110_AABOBQ' 'sip-files00063.jp2'
9b1164ef49ff74df194c414eeb5be00c
bd9c4ecc10d7cab15af4ae96221e31079e131002
describe
'376902' 'info:fdaE20100110_AAACDNfileF20100110_AABOBR' 'sip-files00063.jpg'
09153441425ab0ca8f657daba16607ea
9572f256b918db14f8b258c33985b17b8c15f144
'2012-05-16T11:58:33-04:00'
describe
'28901' 'info:fdaE20100110_AAACDNfileF20100110_AABOBS' 'sip-files00063.pro'
46b3b0ec7c5122a5c1f9eaf2a1ef5666
ea5829fb7683e7c57c0c237ef2b4974102c98068
'2012-05-16T11:57:32-04:00'
describe
'119791' 'info:fdaE20100110_AAACDNfileF20100110_AABOBT' 'sip-files00063.QC.jpg'
78c2b9fae8639ba23067d5bc1251a153
5cf93581c6ced27423f5afa330234f831ec48172
describe
'3705596' 'info:fdaE20100110_AAACDNfileF20100110_AABOBU' 'sip-files00063.tif'
c079d88fcb59a6dee48257d4a2b83829
9c1ba3f094d7a81756d739f9a4e7950bf4c626cb
'2012-05-16T12:00:25-04:00'
describe
'1378' 'info:fdaE20100110_AAACDNfileF20100110_AABOBV' 'sip-files00063.txt'
a3e528dd60b1692f46415d13d707aa2c
6799109ed17a82216bf2ac0c1e996da7f5d6508e
'2012-05-16T12:03:10-04:00'
describe
'34633' 'info:fdaE20100110_AAACDNfileF20100110_AABOBW' 'sip-files00063thm.jpg'
be04b676679b2439e2cef93a1cdaf5a3
de8ccac3b66bbd01d689709b45e5930382b1ff79
'2012-05-16T12:03:29-04:00'
describe
'443925' 'info:fdaE20100110_AAACDNfileF20100110_AABOBX' 'sip-files00064.jp2'
cb3aa7b4b4543c66383a1ab7f24bcc86
7cafecdd91d3974f97b2e3c914e2baa100767268
'2012-05-16T12:05:14-04:00'
describe
'516797' 'info:fdaE20100110_AAACDNfileF20100110_AABOBY' 'sip-files00064.jpg'
601b4cf8b77c03218c1e7509cd2179fb
d7956e445c26e3736df469535eb4d2f599fd42c4
describe
'57968' 'info:fdaE20100110_AAACDNfileF20100110_AABOBZ' 'sip-files00064.pro'
ce3df840d4c694b6f415446c03001495
504897711aaa5b413b1f29857bd33dddf6a1029d
'2012-05-16T12:07:11-04:00'
describe
'170263' 'info:fdaE20100110_AAACDNfileF20100110_AABOCA' 'sip-files00064.QC.jpg'
f031793bcb4384221761e0260c075b9c
dbc65d2d8f9437f11b935e5a1ed9a79f82560f65
'2012-05-16T11:58:02-04:00'
describe
'3554418' 'info:fdaE20100110_AAACDNfileF20100110_AABOCB' 'sip-files00064.tif'
ea5d0c1ae708aab3d6a26624c1a2fc30
43882a9b3bd050141dd440db872218574325f3a3
'2012-05-16T11:59:48-04:00'
describe
'2322' 'info:fdaE20100110_AAACDNfileF20100110_AABOCC' 'sip-files00064.txt'
459ab0848dead457f166e27db9abf7df
f26ffcb0a261b469ea99a9c57750c9599a795f72
'2012-05-16T12:02:42-04:00'
describe
'48268' 'info:fdaE20100110_AAACDNfileF20100110_AABOCD' 'sip-files00064thm.jpg'
902059e93728a437ec9ed9b772c9b2c2
d3239c823459ffad50ade5ea19ce75ad49881695
describe
'450472' 'info:fdaE20100110_AAACDNfileF20100110_AABOCE' 'sip-files00065.jp2'
2102f8aceb08ff0e1d65297f35c4625c
48216dd7c4bd025ccb379650038a1def3dab0931
'2012-05-16T12:05:48-04:00'
describe
'556255' 'info:fdaE20100110_AAACDNfileF20100110_AABOCF' 'sip-files00065.jpg'
af7e07f13ee0fa1c2693bcf87fd17a69
891de305bf6285c3583e31344d5853af86fc4d6f
'2012-05-16T12:05:01-04:00'
describe
'62530' 'info:fdaE20100110_AAACDNfileF20100110_AABOCG' 'sip-files00065.pro'
ba4de911cfda1db40ee60b2b19624282
25bb91d99f4b72bc7949a5146c3aba79c76bc85a
'2012-05-16T12:07:20-04:00'
describe
'177262' 'info:fdaE20100110_AAACDNfileF20100110_AABOCH' 'sip-files00065.QC.jpg'
8561ca23fe2e3ccb0f091814712f755d
846036f3f17655b6a358e3c4f916dd9721120438
'2012-05-16T12:02:08-04:00'
describe
'3606180' 'info:fdaE20100110_AAACDNfileF20100110_AABOCI' 'sip-files00065.tif'
9bbb22469e40baa24ed5e78f1ef218e3
edba5f0c87a04c1ca9a7ea2ab5a089f45a9e0b82
'2012-05-16T11:58:48-04:00'
describe
'2491' 'info:fdaE20100110_AAACDNfileF20100110_AABOCJ' 'sip-files00065.txt'
09b1dc747dc2239fa64aef371e3ab213
bcdb164572df0e10daa9dfe5f0ac0d953fdc7358
'2012-05-16T11:58:15-04:00'
describe
'50902' 'info:fdaE20100110_AAACDNfileF20100110_AABOCK' 'sip-files00065thm.jpg'
ae3846ded604ec3d0441687fae1f2f06
7ad986cc9ea3a83b020ca24e34dbcc795c577ff4
'2012-05-16T11:57:57-04:00'
describe
'462442' 'info:fdaE20100110_AAACDNfileF20100110_AABOCL' 'sip-files00066.jp2'
eab346b2371ed76c70c7f16315c089c9
4ed64f69daacff18f7b59ae88444fd424d488555
'2012-05-16T12:01:07-04:00'
describe
'559467' 'info:fdaE20100110_AAACDNfileF20100110_AABOCM' 'sip-files00066.jpg'
7ce61e07ef4b1b9de56dc1987ceed4a1
85be390352d462f53dcc5e8032645b631d73fcae
'2012-05-16T12:02:10-04:00'
describe
'66271' 'info:fdaE20100110_AAACDNfileF20100110_AABOCN' 'sip-files00066.pro'
1ec6d30ce851572a8bdafe74b9517ba6
aaabb45d405a35368633a4c6222622379ecf3c57
'2012-05-16T11:56:08-04:00'
describe
'181492' 'info:fdaE20100110_AAACDNfileF20100110_AABOCO' 'sip-files00066.QC.jpg'
e2abcb4b4d02f8963da05fc3ab557fa3
1a1ca519ba3d59a8814efdd28287edabc6040b98
'2012-05-16T12:03:39-04:00'
describe
'3701934' 'info:fdaE20100110_AAACDNfileF20100110_AABOCP' 'sip-files00066.tif'
2eebebc9dc87fee548bd84ec063172e2
d721b5d0fb34ea3dc9516a85df6b8df824009bd4
'2012-05-16T11:57:21-04:00'
describe
'2619' 'info:fdaE20100110_AAACDNfileF20100110_AABOCQ' 'sip-files00066.txt'
4411c51d6b1c6ea21013484f12469589
9c25e06621ec30de74a87c24f95bf55add404834
'2012-05-16T11:57:10-04:00'
describe
'47694' 'info:fdaE20100110_AAACDNfileF20100110_AABOCR' 'sip-files00066thm.jpg'
c8a32f008f019bfebd8181b967aab637
e261983314052920e34f6ca8933370a2799a6504
describe
'463038' 'info:fdaE20100110_AAACDNfileF20100110_AABOCS' 'sip-files00067.jp2'
6786b8f08e36adf0a33a6fab4f061938
4a0415023cb0c26b1ea0457144b1cde1d1205897
'2012-05-16T12:04:04-04:00'
describe
'497626' 'info:fdaE20100110_AAACDNfileF20100110_AABOCT' 'sip-files00067.jpg'
abe4be9f30299d73b77e57f9d55b9f46
b4f6612cf56e2b031a4f38caa17e20420439209b
'2012-05-16T12:04:24-04:00'
describe
'32790' 'info:fdaE20100110_AAACDNfileF20100110_AABOCU' 'sip-files00067.pro'
da08f84c7546cb051500406c45b13c33
e8386b1a36ef5cfad405f719abb38d0a1a9dd7b3
describe
'153210' 'info:fdaE20100110_AAACDNfileF20100110_AABOCV' 'sip-files00067.QC.jpg'
de4c549484f315ecf274441c8dc16a0f
0451dcc7281774d0dd9e47bc3c0ea3531cce310a
'2012-05-16T12:06:53-04:00'
describe
'3707050' 'info:fdaE20100110_AAACDNfileF20100110_AABOCW' 'sip-files00067.tif'
61debe5622a517e713322b3295912f64
fb3d534ace78ec59947ce42cf881cafa4f52fe94
'2012-05-16T12:01:35-04:00'
describe
'1331' 'info:fdaE20100110_AAACDNfileF20100110_AABOCX' 'sip-files00067.txt'
53d41ef116e80cbe1f3a4f847a77035d
9587cd431196f90e0f5586c4035d3874f438ad5b
describe
'42993' 'info:fdaE20100110_AAACDNfileF20100110_AABOCY' 'sip-files00067thm.jpg'
356964ef6430af4c51d35efadf61e3e8
09b8eb76d8a7b124740d260f830b51e2a11e0dd3
'2012-05-16T12:02:34-04:00'
describe
'456150' 'info:fdaE20100110_AAACDNfileF20100110_AABOCZ' 'sip-files00068.jp2'
a2ef13ba001123102f6bb4a991394c45
49beae22b303d4f19c6b4ea84f8360969bee0276
describe
'550794' 'info:fdaE20100110_AAACDNfileF20100110_AABODA' 'sip-files00068.jpg'
6c40329fde45c9636989ce8aa5bc37f1
52680ae628e88050b58cd43934fd6922d74ccbce
describe
'64055' 'info:fdaE20100110_AAACDNfileF20100110_AABODB' 'sip-files00068.pro'
01bc8e466162d796e7fe70cbf91ee0de
a92f4b6bb49c298222e5c797570193284ba06857
describe
'177947' 'info:fdaE20100110_AAACDNfileF20100110_AABODC' 'sip-files00068.QC.jpg'
3bcd5d06053621cdd1f187fb9b05d443
7bb114e303e1414da2f83827a632b3eeed4de72b
'2012-05-16T11:57:04-04:00'
describe
'3651550' 'info:fdaE20100110_AAACDNfileF20100110_AABODD' 'sip-files00068.tif'
0a30598e1e6ffd2a9898191c08057df6
8a104c0ea57c2ff94f187f541d98113d749952ed
'2012-05-16T12:01:28-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABODE' 'sip-files00068.txt'
3b9f1aadb52799960576c956d0ab1382
183412d5506ff475f1f2fb6b48583b03e9073273
'2012-05-16T11:58:42-04:00'
describe
'50601' 'info:fdaE20100110_AAACDNfileF20100110_AABODF' 'sip-files00068thm.jpg'
014cfa4bd301d6804c8eb2b8fed197d6
9846d53b7590119b262b65d0800403fb27658e83
describe
'465601' 'info:fdaE20100110_AAACDNfileF20100110_AABODG' 'sip-files00069.jp2'
9b2f648acedf9e0c0f644fb32ef954b4
65db939a0fbbe7fe23f95e85f29231dd332e4447
describe
'562164' 'info:fdaE20100110_AAACDNfileF20100110_AABODH' 'sip-files00069.jpg'
c7c11c2bcd708531a70880f499a1b3cd
33e1e77907ad7588768cc6380d73cbd9af4be76b
describe
'59097' 'info:fdaE20100110_AAACDNfileF20100110_AABODI' 'sip-files00069.pro'
5258649919960ed6e8503ba5338c931b
ccf63249363c07f2cef2174c999b3c27806efb66
describe
'179686' 'info:fdaE20100110_AAACDNfileF20100110_AABODJ' 'sip-files00069.QC.jpg'
0b5d6e7516fda4c542349b5eb7066177
7e53fd88a6e53d1df685ee9d66176fb2d393721a
'2012-05-16T12:00:15-04:00'
describe
'3727100' 'info:fdaE20100110_AAACDNfileF20100110_AABODK' 'sip-files00069.tif'
d6259149e1ba5ccc4b87f7617ffca984
2d91500bbc6475d9332dac3057fb94bffb1c4e3a
'2012-05-16T12:00:42-04:00'
describe
'2371' 'info:fdaE20100110_AAACDNfileF20100110_AABODL' 'sip-files00069.txt'
69bede1bf2389b0a29745069cabf186f
4e3d70457a4a4b6a3bb51e79cedf4b58283fba21
'2012-05-16T12:01:29-04:00'
describe
'48631' 'info:fdaE20100110_AAACDNfileF20100110_AABODM' 'sip-files00069thm.jpg'
bd5f75a646fc7c51863a0625ecb5677c
c59676687048c12f34ac083bdc91113cc03be516
describe
'470945' 'info:fdaE20100110_AAACDNfileF20100110_AABODN' 'sip-files00070.jp2'
2fcc983636cf1fd0819f43e844337627
781c3b778a2477844af966bf65776f48565d9ff6
'2012-05-16T11:58:54-04:00'
describe
'473433' 'info:fdaE20100110_AAACDNfileF20100110_AABODO' 'sip-files00070.jpg'
85589b4e7450f7222df8aa9ed68da541
18ce0309249e7b54736e902b11a00ed021898e49
describe
'35445' 'info:fdaE20100110_AAACDNfileF20100110_AABODP' 'sip-files00070.pro'
0411d51e8cef8e8b9a94f4634498bee2
935c524df2f77a9193c0e88226c52e03c38925c6
describe
'149384' 'info:fdaE20100110_AAACDNfileF20100110_AABODQ' 'sip-files00070.QC.jpg'
3f058b6dc828aa351a68fe883053d5d1
1e4460408c5100ef4d477cf1a8021f9ef4f31c70
'2012-05-16T11:56:54-04:00'
describe
'3772116' 'info:fdaE20100110_AAACDNfileF20100110_AABODR' 'sip-files00070.tif'
6fab23bd3ed725a67a50b99ef39e8939
d2bf801b843037d61e2658be8fcdacc837191e6a
'2012-05-16T12:02:05-04:00'
describe
'1516' 'info:fdaE20100110_AAACDNfileF20100110_AABODS' 'sip-files00070.txt'
05681ada12d72db61ad3f4f27477fafd
3b9a8a263677af68aa1d00b58058f84b1ca69f5b
describe
'41114' 'info:fdaE20100110_AAACDNfileF20100110_AABODT' 'sip-files00070thm.jpg'
277fcdf99b87982136fe568ad6c2411f
15e9613a154d0b4760e6c6b04efd2b78280b04b4
'2012-05-16T11:59:43-04:00'
describe
'468390' 'info:fdaE20100110_AAACDNfileF20100110_AABODU' 'sip-files00071.jp2'
06624c748fb341d3896f248e19499dce
3d1d4740fa9b344270ffb716d86664abf8b7e77a
describe
'576443' 'info:fdaE20100110_AAACDNfileF20100110_AABODV' 'sip-files00071.jpg'
3323de100bc1a9883cafb337648178a0
503409d4636e3e270dde6b2865e97473e73f9e17
'2012-05-16T12:00:30-04:00'
describe
'61058' 'info:fdaE20100110_AAACDNfileF20100110_AABODW' 'sip-files00071.pro'
f8a2e8a8598a39c8281aab000ac60807
92d9b48efde8efcc74aa577b805181aacd0220b8
'2012-05-16T12:01:13-04:00'
describe
'180842' 'info:fdaE20100110_AAACDNfileF20100110_AABODX' 'sip-files00071.QC.jpg'
d49e74350874480fdccbc499a83cae9e
4e07e7509c16572fd1232ad609b6f7c148576b84
'2012-05-16T12:06:01-04:00'
describe
'3749498' 'info:fdaE20100110_AAACDNfileF20100110_AABODY' 'sip-files00071.tif'
ff2e5d1e1642cdab4a538eec16dfb49c
d7a0cc08c4bcdb292d240bf1b8da65aafa9f3c4e
'2012-05-16T12:00:23-04:00'
describe
'2430' 'info:fdaE20100110_AAACDNfileF20100110_AABODZ' 'sip-files00071.txt'
06cc5f5ecad5e012bf9c7377b7c0b3f1
524d8563bd804fcc0f70e3222ad4675e492d6a35
'2012-05-16T12:05:18-04:00'
describe
'49023' 'info:fdaE20100110_AAACDNfileF20100110_AABOEA' 'sip-files00071thm.jpg'
21d74705180a28ed2f44932deb1d4baa
00e4a5e7cd7fc7bcfa8e32691825c0635e6dc1f2
'2012-05-16T11:57:53-04:00'
describe
'474633' 'info:fdaE20100110_AAACDNfileF20100110_AABOEB' 'sip-files00072.jp2'
d90661c051881584e1669211861b97a1
b6bb7939091fd2c5bc9a6926c22e932420b695f8
describe
'486164' 'info:fdaE20100110_AAACDNfileF20100110_AABOEC' 'sip-files00072.jpg'
62da38d3ecbdb649a0a739fb031d97b6
9099d0f6e5f5113f49247a40df3338a0cc27db0d
'2012-05-16T12:05:59-04:00'
describe
'8517' 'info:fdaE20100110_AAACDNfileF20100110_AABOED' 'sip-files00072.pro'
ae77678e63fe6abdd9e6bc9d54f76d44
7e4a31dabb275b6aa5ae7f9257b5e7df8a7d3e68
'2012-05-16T11:58:11-04:00'
describe
'145216' 'info:fdaE20100110_AAACDNfileF20100110_AABOEE' 'sip-files00072.QC.jpg'
63ad1cf41fd149934e162daaed126aac
ccce15e191fcc3e9bdfdb8b53233f0e16e922185
describe
'3800718' 'info:fdaE20100110_AAACDNfileF20100110_AABOEF' 'sip-files00072.tif'
59bb070a7b97d29a497d13bcabc7dcfb
5cd3dfe986a877670939105114f1adc31cc63df8
'2012-05-16T12:04:03-04:00'
describe
'378' 'info:fdaE20100110_AAACDNfileF20100110_AABOEG' 'sip-files00072.txt'
ccab722299761413128b814526b28ca0
e05d30c6ce64ec2cbce420b890da6b612ef59213
'2012-05-16T12:05:46-04:00'
describe
Invalid character
'39744' 'info:fdaE20100110_AAACDNfileF20100110_AABOEH' 'sip-files00072thm.jpg'
6abd3c14ec3f81558c236fd10a852957
9357411939e18b9234d8816fd2203ecf13c9088b
'2012-05-16T11:56:26-04:00'
describe
'461868' 'info:fdaE20100110_AAACDNfileF20100110_AABOEI' 'sip-files00073.jp2'
ebd7dda602cbbce8e14ba4c409b8575d
e82c37bbedc1f7be1cd6df1e80f62d3c37e36c87
'2012-05-16T12:04:30-04:00'
describe
'587417' 'info:fdaE20100110_AAACDNfileF20100110_AABOEJ' 'sip-files00073.jpg'
606409fa7fd0f29ba1db2d0e0a01162c
d086fc4850ba57e9903bd5af7ceb5573bb976a73
'2012-05-16T11:59:28-04:00'
describe
'65560' 'info:fdaE20100110_AAACDNfileF20100110_AABOEK' 'sip-files00073.pro'
86de52e4406024eff7b52e7cc5baf209
e3ef17db1669bdcd1913008e26d87d8e327f8a85
'2012-05-16T11:58:23-04:00'
describe
'190114' 'info:fdaE20100110_AAACDNfileF20100110_AABOEL' 'sip-files00073.QC.jpg'
7ce4073170517f57b836a6b2d7e2d313
7d4abb4ab0335262db5f4233a3b26e611cf5578c
'2012-05-16T11:59:04-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABOEM' 'sip-files00073.tif'
995480af9867e04bd99915c2735055bd
2918038580554cb961ed50e41b6ba259fd680178
'2012-05-16T12:01:42-04:00'
describe
'2600' 'info:fdaE20100110_AAACDNfileF20100110_AABOEN' 'sip-files00073.txt'
cbdbf14e08499a0e0a675f7d2bd100b6
84d7b641288169e9bcb3de5438ae410ecd40d5b3
'2012-05-16T12:03:33-04:00'
describe
'49596' 'info:fdaE20100110_AAACDNfileF20100110_AABOEO' 'sip-files00073thm.jpg'
ff9f5d65d88bd17f434948aeaceeee56
d8f281ac7d3162a9dd15fbe9e93f52d99d18fdc1
describe
'462856' 'info:fdaE20100110_AAACDNfileF20100110_AABOEP' 'sip-files00074.jp2'
b123d1b6cddd74d4a4873f90977787d0
f3238d21532a37ca7e04222063bf036a5ed61aee
'2012-05-16T12:03:41-04:00'
describe
'595817' 'info:fdaE20100110_AAACDNfileF20100110_AABOEQ' 'sip-files00074.jpg'
8d3171b1a4c9095c5c9e59d61b433dba
878e16236874a10c332470084d74cd660d0f553b
'2012-05-16T12:03:31-04:00'
describe
'69984' 'info:fdaE20100110_AAACDNfileF20100110_AABOER' 'sip-files00074.pro'
6912eddce20f950c37abe565caa390e9
f11871e47cc01368a7dffc418448875a2fd92513
'2012-05-16T11:59:24-04:00'
describe
'193748' 'info:fdaE20100110_AAACDNfileF20100110_AABOES' 'sip-files00074.QC.jpg'
eefba23837fbd4a1fa17855262dcdf72
738657b37c382bd7c6f5e381e665b7b38e563227
'2012-05-16T11:56:34-04:00'
describe
'3705366' 'info:fdaE20100110_AAACDNfileF20100110_AABOET' 'sip-files00074.tif'
c7ad065dccc4b20d75b0a77843dee3f5
c68cc7154443ee311d816d7ed8c5d012ad149859
'2012-05-16T12:04:50-04:00'
describe
'2751' 'info:fdaE20100110_AAACDNfileF20100110_AABOEU' 'sip-files00074.txt'
49aa6e2371d837d13a245db70d4fab20
bd096a71e67b25516a6cf1a7000727c3590abfc2
describe
'48565' 'info:fdaE20100110_AAACDNfileF20100110_AABOEV' 'sip-files00074thm.jpg'
7b792334a687268a7b5647c361eac1fa
7bd111345511bc43fc8ee300a766306a71c24759
describe
'469877' 'info:fdaE20100110_AAACDNfileF20100110_AABOEW' 'sip-files00075.jp2'
ffdf8462eb5900fa657303e1ea555321
a0591ba46cf07fd266fb5bcffdcd29f4739cfea0
'2012-05-16T12:02:04-04:00'
describe
'181984' 'info:fdaE20100110_AAACDNfileF20100110_AABOEX' 'sip-files00075.jpg'
95b04a395f7436a83f9c2cbd5a871ac9
f623be53097daf7937650069146055a1e9716252
'2012-05-16T12:06:36-04:00'
describe
'22827' 'info:fdaE20100110_AAACDNfileF20100110_AABOEY' 'sip-files00075.pro'
0da7d5a9ca671137b7448a88503af860
9634acca5a2ed82b4b6315e0b0762a1fc348ab40
describe
'64382' 'info:fdaE20100110_AAACDNfileF20100110_AABOEZ' 'sip-files00075.QC.jpg'
fc87f9f63a50d1ae5be879f165061aae
66029aceade66a3c4553deb21524044c845d9f6d
'2012-05-16T11:56:27-04:00'
describe
'3536476' 'info:fdaE20100110_AAACDNfileF20100110_AABOFA' 'sip-files00075.tif'
12fdab9f8393d5837eea45b376e32cd5
81cf453557255f7eefcdf5a112832bf3774e1656
'2012-05-16T12:06:13-04:00'
describe
'1105' 'info:fdaE20100110_AAACDNfileF20100110_AABOFB' 'sip-files00075.txt'
2a8dd83960adc75fcb8fb7fee190afcb
90e46ec48d0beeed4aec2cffc136227c86dab2f5
'2012-05-16T12:06:47-04:00'
describe
'26696' 'info:fdaE20100110_AAACDNfileF20100110_AABOFC' 'sip-files00075thm.jpg'
0c9e5c1d7967b7392d813588951be38a
7ca53d4a0a0552ed7dcf9d83029c4846e3cd2794
describe
'502711' 'info:fdaE20100110_AAACDNfileF20100110_AABOFD' 'sip-files00076.jp2'
efe1dc263544bfd6f2230929e334e19c
bdc78c46ee2fce0713527f66dae408e12114381e
describe
'597605' 'info:fdaE20100110_AAACDNfileF20100110_AABOFE' 'sip-files00076.jpg'
474dc9eae9c70e0e08832b321f2d8cf7
0b911bb3c986abcebaebd474ebcc2375d4974ddb
'2012-05-16T12:05:00-04:00'
describe
'67583' 'info:fdaE20100110_AAACDNfileF20100110_AABOFF' 'sip-files00076.pro'
10665b672bd8cd28e7ffdf02b4a62ebe
6905564d71443047ab84b965b9314f0db6693dbd
'2012-05-16T11:58:59-04:00'
describe
'188059' 'info:fdaE20100110_AAACDNfileF20100110_AABOFG' 'sip-files00076.QC.jpg'
1a4024a95bf46b0ce4dc41a439aff38f
2801740cc6f57dcbf274f1af4ce620dd2223a530
'2012-05-16T11:56:05-04:00'
describe
'4024406' 'info:fdaE20100110_AAACDNfileF20100110_AABOFH' 'sip-files00076.tif'
828f8eb4981b576284664dd04aaa09b9
21fd51fd197c16ca507fb3a6e86038b9e6eb7567
describe
'2657' 'info:fdaE20100110_AAACDNfileF20100110_AABOFI' 'sip-files00076.txt'
57e88d552a771c5285a00e5522125f2c
a10f195429410ac61a92ccbfa6478cea69f269fa
describe
'49221' 'info:fdaE20100110_AAACDNfileF20100110_AABOFJ' 'sip-files00076thm.jpg'
f742df0eb51c903e197d9c202e29f20d
39e9e3ee35547e7ba70d9fcfb9ee48b42da997a4
describe
'491195' 'info:fdaE20100110_AAACDNfileF20100110_AABOFK' 'sip-files00077.jp2'
43ad5e93a0a55c5ce6b64d2bd2b0075c
f167be631bc67a31f9c8d0551ea0bd77edcc63ba
'2012-05-16T11:57:27-04:00'
describe
'546427' 'info:fdaE20100110_AAACDNfileF20100110_AABOFL' 'sip-files00077.jpg'
bf6d4ef63c91d4c16713d7ffb06087c6
00acdde4317379acba7944bfc4e96c60d4d0096f
describe
'59034' 'info:fdaE20100110_AAACDNfileF20100110_AABOFM' 'sip-files00077.pro'
8866e2496dc318a1a8ad72f5201d5e09
fe2bf0788cacf42aa349ceb4bf3b5cfcc5303049
'2012-05-16T12:03:27-04:00'
describe
'171137' 'info:fdaE20100110_AAACDNfileF20100110_AABOFN' 'sip-files00077.QC.jpg'
74b207246ef2af0c4edac838206f4086
2ee7c08cf6e1921d39350c3e524275b7b80452b2
'2012-05-16T12:03:38-04:00'
describe
'3932034' 'info:fdaE20100110_AAACDNfileF20100110_AABOFO' 'sip-files00077.tif'
5969aef2d7668ce98c8fcf8e8352d2ed
e2a194c31a96673d512f85596cb50a55c15474a5
describe
'2350' 'info:fdaE20100110_AAACDNfileF20100110_AABOFP' 'sip-files00077.txt'
aad7cf66e4284f0480e6fd3bda32a9d5
fa29a29170f062374c3608e5bb24e34571085e17
'2012-05-16T12:02:27-04:00'
describe
'47372' 'info:fdaE20100110_AAACDNfileF20100110_AABOFQ' 'sip-files00077thm.jpg'
974059de23f923520fd34db186a4dfea
86a781529e85bbab7349cf9bd7cb7db641c4e502
describe
'492863' 'info:fdaE20100110_AAACDNfileF20100110_AABOFR' 'sip-files00078.jp2'
d8fe48ce0c83cd819d8c46f6cc1271e7
e256752ff211bc5144883c71a1a4749451bbb48d
'2012-05-16T12:00:59-04:00'
describe
'189215' 'info:fdaE20100110_AAACDNfileF20100110_AABOFS' 'sip-files00078.jpg'
738608b0727147b1669f891b20f9007b
527db6de43fc4cacae548d1630f174287797d7d6
'2012-05-16T11:57:41-04:00'
describe
'11762' 'info:fdaE20100110_AAACDNfileF20100110_AABOFT' 'sip-files00078.pro'
b67ab90c399d795582d9e6ca679d90ea
fa353d0bf41ae3ca3a1963270e985bbee0eadad8
describe
'65173' 'info:fdaE20100110_AAACDNfileF20100110_AABOFU' 'sip-files00078.QC.jpg'
7cfd094831ae82cdb0a63c122f00b8f9
b4bae145c0223fbc05ef5ca980be9cbc5ff978cf
describe
'4300568' 'info:fdaE20100110_AAACDNfileF20100110_AABOFV' 'sip-files00078.tif'
72a8dad9c336c034e0d14d93ddae3d49
96befce55d1fa02acb38816bd3c5dee02aa4bf60
describe
'695' 'info:fdaE20100110_AAACDNfileF20100110_AABOFW' 'sip-files00078.txt'
39ead9016ec75d627b3a12dc0c325d3b
889bc8bd26f5e44cdad3bc0d429b08194ac2bdb3
'2012-05-16T12:06:06-04:00'
describe
'27614' 'info:fdaE20100110_AAACDNfileF20100110_AABOFX' 'sip-files00078thm.jpg'
88750b9b7cd2a5d376059baf58ad2baf
563ec5b8733b029f0a1fdd0eaccc29f88895bc16
'2012-05-16T12:01:18-04:00'
describe
'507773' 'info:fdaE20100110_AAACDNfileF20100110_AABOFY' 'sip-files00079.jp2'
e159408de4da9e45e54536a06284ba35
6edf9290a7d2a64609ee4ee3399822a15335902d
'2012-05-16T12:02:35-04:00'
describe
'556399' 'info:fdaE20100110_AAACDNfileF20100110_AABOFZ' 'sip-files00079.jpg'
e0524c2bfcd3638c4bfe4078e606302f
bee16d5d132e535f0f132448e5e9e0ee97f9d39b
describe
'65457' 'info:fdaE20100110_AAACDNfileF20100110_AABOGA' 'sip-files00079.pro'
4a304539ff5dd0cd3917e457185e29f9
2c2a8fe77fd3f5a1f508dfdd65cf7fdb84aeba8d
'2012-05-16T12:00:18-04:00'
describe
'175171' 'info:fdaE20100110_AAACDNfileF20100110_AABOGB' 'sip-files00079.QC.jpg'
36eb8e65121e2502574756dc89dd04df
80a9d478819d1aaa2ec7b96ff8e0fe20edbdd4b4
'2012-05-16T11:56:59-04:00'
describe
'4064618' 'info:fdaE20100110_AAACDNfileF20100110_AABOGC' 'sip-files00079.tif'
d155a0cd9f8a2d298173110a6452a014
62ceb9ce2d778684c9194d226c19a010cbf70d7a
'2012-05-16T12:03:12-04:00'
describe
'2626' 'info:fdaE20100110_AAACDNfileF20100110_AABOGD' 'sip-files00079.txt'
3bc887dc166535b97927a9e6aefdbb47
a1f0e1e12f9089278d094b45d31e6806da9e2754
describe
'45837' 'info:fdaE20100110_AAACDNfileF20100110_AABOGE' 'sip-files00079thm.jpg'
ef5e9c80fa8f4fbd967083da02bfe77c
3739103da3177322234765f3a4361336ae930dbe
describe
'494774' 'info:fdaE20100110_AAACDNfileF20100110_AABOGF' 'sip-files00080.jp2'
f34f0930a07f733fd44266d472525f65
474af41428c49ebbd6eb06fc55668d6f1537ba99
describe
'595929' 'info:fdaE20100110_AAACDNfileF20100110_AABOGG' 'sip-files00080.jpg'
5e72cc576492e8a4183366038cdd6d5d
fc970ede96918368dc2c88c593c7a9b292a87fd7
'2012-05-16T12:06:43-04:00'
describe
'65936' 'info:fdaE20100110_AAACDNfileF20100110_AABOGH' 'sip-files00080.pro'
939b54614a933f5cb2bd624070f0ba31
a5584a5ceeb025e0c6daddeb783651225877bb55
'2012-05-16T12:02:48-04:00'
describe
'183560' 'info:fdaE20100110_AAACDNfileF20100110_AABOGI' 'sip-files00080.QC.jpg'
a4d06d8c8583eb6e700d622b7c631231
a247c992e65df889da59c265b9fd0e149c301815
describe
'3961166' 'info:fdaE20100110_AAACDNfileF20100110_AABOGJ' 'sip-files00080.tif'
91264712f26217add5a4c348b0a3c380
186e87616153f13bec2bdb831449eef6cda412c2
'2012-05-16T12:05:28-04:00'
describe
'2601' 'info:fdaE20100110_AAACDNfileF20100110_AABOGK' 'sip-files00080.txt'
ea59ca288ad7359ccc6650f3489e3a9e
4cda8a7845538ce5c1b608366481467acf530aec
describe
'48717' 'info:fdaE20100110_AAACDNfileF20100110_AABOGL' 'sip-files00080thm.jpg'
16e5613bc3d4d1ede0d256cd5e713219
e041ef4a8e4bf8a6b66613ff36ef55930e643691
describe
'499783' 'info:fdaE20100110_AAACDNfileF20100110_AABOGM' 'sip-files00081.jp2'
b8a0e03f3dd4a1e297de7b745bf65be0
699a38ca2f0178afe411c410f4884b25b6e4cd95
'2012-05-16T11:58:37-04:00'
describe
'578987' 'info:fdaE20100110_AAACDNfileF20100110_AABOGN' 'sip-files00081.jpg'
aa43406a2389775dfe318d27d40e1aef
4cd04754960f733a62dbe821cdcd17b031dcda64
'2012-05-16T12:06:16-04:00'
describe
'67242' 'info:fdaE20100110_AAACDNfileF20100110_AABOGO' 'sip-files00081.pro'
fb8e0081f431b2d8db778b05ffff8353
f40f5d372751653f584a916804bd86e5f522789c
describe
'185526' 'info:fdaE20100110_AAACDNfileF20100110_AABOGP' 'sip-files00081.QC.jpg'
dda9b43b624e47accf5426d90816654a
eeee118a7be8518cff94c021c22dd55652bcf699
'2012-05-16T12:07:12-04:00'
describe
'4000690' 'info:fdaE20100110_AAACDNfileF20100110_AABOGQ' 'sip-files00081.tif'
9cec3b5a39ac3a2193cf2eb968f05ce9
ee5d9b31bbcbceffde2f3a19aadf8d4353b5506e
'2012-05-16T11:57:37-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABOGR' 'sip-files00081.txt'
b809fac80f4ca6a3f52fde536fa9c7b1
18d509e9466ccee7743b6ff1a9c04220233f6a5e
'2012-05-16T11:58:21-04:00'
describe
'48001' 'info:fdaE20100110_AAACDNfileF20100110_AABOGS' 'sip-files00081thm.jpg'
f5eed2752e1e2c5199f4efed8b50bbbb
c658c8d522bcce9df781597ebcc52a2b27aac684
'2012-05-16T12:00:28-04:00'
describe
'487085' 'info:fdaE20100110_AAACDNfileF20100110_AABOGT' 'sip-files00082.jp2'
686228da7fb4685f5df8fb5796be284a
26724370b0de34a9c89c946ffe1f15965756c0b6
'2012-05-16T12:01:49-04:00'
describe
'551827' 'info:fdaE20100110_AAACDNfileF20100110_AABOGU' 'sip-files00082.jpg'
a4cdb5539fc9ac81f477ff2f5cb4fb0d
d36030b9c5b740989753d7f83cd2566a64dac12a
'2012-05-16T12:05:12-04:00'
describe
'62170' 'info:fdaE20100110_AAACDNfileF20100110_AABOGV' 'sip-files00082.pro'
66db103afa736cc0648ed857be4688bc
eedb37c8a954ccfd3e1b77d4be01c0660accf32b
describe
'176196' 'info:fdaE20100110_AAACDNfileF20100110_AABOGW' 'sip-files00082.QC.jpg'
9a153086e0afe7f7adec0d63304bb746
b323a2360696c68a6226fe8455363d654eab2c5f
'2012-05-16T12:01:51-04:00'
describe
'3899098' 'info:fdaE20100110_AAACDNfileF20100110_AABOGX' 'sip-files00082.tif'
2ff28cb01b935f98280ece0a1aab4eae
76716888c7a150e0e78cc2d951aa177dc74f5577
'2012-05-16T12:03:24-04:00'
describe
'2484' 'info:fdaE20100110_AAACDNfileF20100110_AABOGY' 'sip-files00082.txt'
8d9532e48346552f5c0c9eef476d92c8
da91fea8cbd914197d803471dfbdb4becd1ba3b3
'2012-05-16T11:59:08-04:00'
describe
'46308' 'info:fdaE20100110_AAACDNfileF20100110_AABOGZ' 'sip-files00082thm.jpg'
39ca1b97e9f007d39849aecb34c95b21
d6f8b6707b2eddd3411fca5331f6d974405470bb
'2012-05-16T12:06:41-04:00'
describe
'482735' 'info:fdaE20100110_AAACDNfileF20100110_AABOHA' 'sip-files00083.jp2'
4ebd2e76517b131393bb9e1f8a7a13ab
7072e0a54cb81fa0a980500af7d7d5ab937cdcca
'2012-05-16T12:03:49-04:00'
describe
'594424' 'info:fdaE20100110_AAACDNfileF20100110_AABOHB' 'sip-files00083.jpg'
68793f40e92911c0a94d3d0b6cd03d5e
8df36dc1c77b75dd2fbb1f07c98830e0516bb826
describe
'67241' 'info:fdaE20100110_AAACDNfileF20100110_AABOHC' 'sip-files00083.pro'
1b055e2a2dfe9cd416f2bc824c602b75
6e2d81dc5925f4b7e398031fa5500375ad0f67e3
describe
'190406' 'info:fdaE20100110_AAACDNfileF20100110_AABOHD' 'sip-files00083.QC.jpg'
11752c55e53a64ac90fdf4cdd157c921
b882a3fc1bbf5931a151c26a650c4f06e17de2ad
'2012-05-16T11:56:28-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABOHE' 'sip-files00083.tif'
94cf294a57950ed3ad83fc1ceaa16103
054bcbbff55cf439271074618252491acc88f7a9
describe
'2673' 'info:fdaE20100110_AAACDNfileF20100110_AABOHF' 'sip-files00083.txt'
70b7e470b9de6f721410a4475be30ff7
26ccf705b1868c46cbaba03b99c0023ec574de30
describe
'info:fdaE20100110_AAACDNfileF20100110_AABOHG' 'sip-files00083thm.jpg'
001440f7337f8c39ca6fcdf0f7adeef4
c1be3fe199aaac52f986128d4602502984ab4909
'2012-05-16T12:05:23-04:00'
describe
'492806' 'info:fdaE20100110_AAACDNfileF20100110_AABOHH' 'sip-files00084.jp2'
03f1faa3da9bd0ae400a5ec4ac27e5d5
535943edc5c1024af6e72e811d3a1d9ba7db7b23
'2012-05-16T12:01:37-04:00'
describe
'557276' 'info:fdaE20100110_AAACDNfileF20100110_AABOHI' 'sip-files00084.jpg'
e76708daeb2eaf0176cc0c56b26d8ecb
f9f6faad1d07ecd8a1b7b47b2e70649fe03d4083
describe
'64901' 'info:fdaE20100110_AAACDNfileF20100110_AABOHJ' 'sip-files00084.pro'
3e09b29adb786be562bf880a6bb56e18
75ce5a6bb390e6af3095a31915b20d19f0b36341
describe
'179033' 'info:fdaE20100110_AAACDNfileF20100110_AABOHK' 'sip-files00084.QC.jpg'
b34636e96c1431dce0eba8cac2f75785
bb04050dbd40066fe5dc0d565915168f8d7cbdd6
'2012-05-16T12:01:09-04:00'
describe
'3945216' 'info:fdaE20100110_AAACDNfileF20100110_AABOHL' 'sip-files00084.tif'
d81466712ec0b1b4dfa9e772ea02109f
2735c6176a203d58a63894ffec1d15f52b174d72
describe
'2566' 'info:fdaE20100110_AAACDNfileF20100110_AABOHM' 'sip-files00084.txt'
a1121f86cd656b581295332967021906
510543d363b88b68095c4d9abf6e5185e548533f
describe
'48585' 'info:fdaE20100110_AAACDNfileF20100110_AABOHN' 'sip-files00084thm.jpg'
1bd63ecabbabbeb58eb246e920fe7d82
396d5abe46f68fc4193a72f3c6cd983d1f3f786b
'2012-05-16T12:05:21-04:00'
describe
'503476' 'info:fdaE20100110_AAACDNfileF20100110_AABOHO' 'sip-files00085.jp2'
7d1cbfefe2d93b662c44ea093f10178f
bb742ace93c900abf6960ef415b55393291c5ced
'2012-05-16T12:03:53-04:00'
describe
'593408' 'info:fdaE20100110_AAACDNfileF20100110_AABOHP' 'sip-files00085.jpg'
f8901256f962387f4b6c828c0fd68c32
b128eb0031f6410cd3de3728c800f805b224d0d4
describe
'66710' 'info:fdaE20100110_AAACDNfileF20100110_AABOHQ' 'sip-files00085.pro'
e89a7102f1b9a7ed50901d046c8daa71
bc7d167080bec368fd18fa00b9cc455b65966f1f
describe
'183824' 'info:fdaE20100110_AAACDNfileF20100110_AABOHR' 'sip-files00085.QC.jpg'
e65cb79aa5bd3239378b139956d05662
5049a67a25ee7dd5eb42d6e89a66994c93189330
'2012-05-16T12:01:05-04:00'
describe
'4030458' 'info:fdaE20100110_AAACDNfileF20100110_AABOHS' 'sip-files00085.tif'
61d46f0f115951fc1a101e952be706f7
f0895427dff3780c3a029412443889573a06cccc
describe
'2632' 'info:fdaE20100110_AAACDNfileF20100110_AABOHT' 'sip-files00085.txt'
6233495bd79ec3d598c8f2200ea2dd9c
0c14d5d083c149133d19209fcfcb9178ddb622e0
'2012-05-16T11:56:30-04:00'
describe
'48264' 'info:fdaE20100110_AAACDNfileF20100110_AABOHU' 'sip-files00085thm.jpg'
51a79db90cb4eeaab9789423c7ea0e07
6bd8ab4a250f82cc82491a59a0f544c3532ed3be
'2012-05-16T12:06:52-04:00'
describe
'458383' 'info:fdaE20100110_AAACDNfileF20100110_AABOHV' 'sip-files00086.jp2'
7041275e2e6c17afb138409543fa66db
52e99987dcd8f18a973b487b003681435e389e3c
describe
'438431' 'info:fdaE20100110_AAACDNfileF20100110_AABOHW' 'sip-files00086.jpg'
da7fa92f9cf373ae7e59b2ec100601e2
e2132bee8f26dc479562e0d6398fdde368703c55
'2012-05-16T11:57:03-04:00'
describe
'7834' 'info:fdaE20100110_AAACDNfileF20100110_AABOHX' 'sip-files00086.pro'
cd19e0d08e771b4d4b7b1e1e8d6a41c6
c87cb86303f30830ef3b135303612afe5b9c53ec
'2012-05-16T11:56:36-04:00'
describe
'142059' 'info:fdaE20100110_AAACDNfileF20100110_AABOHY' 'sip-files00086.QC.jpg'
93de48582ff74ee93209c4b075f41354
305576ed740d4a097f85eb9297b6775eea3aa9e4
describe
'3669478' 'info:fdaE20100110_AAACDNfileF20100110_AABOHZ' 'sip-files00086.tif'
8f67906b7aae907f312ce1e98a73c3d1
29361ba17cbe19705e54ed67bdc52fe5fd5e8465
describe
'451' 'info:fdaE20100110_AAACDNfileF20100110_AABOIA' 'sip-files00086.txt'
1f8015817c5aca6e41c3cb93934880dd
0ebc7768ba896349070bb5165f5bc45243cda1eb
'2012-05-16T12:00:24-04:00'
describe
'41542' 'info:fdaE20100110_AAACDNfileF20100110_AABOIB' 'sip-files00086thm.jpg'
32cb6b01842213e38f35deb14872bdee
42513f48da2fdb061fa5cf03d020a9636135473d
describe
'459582' 'info:fdaE20100110_AAACDNfileF20100110_AABOIC' 'sip-files00087.jp2'
23aabe6d705d1165394d434c06623076
f6394cfc2550768949e7fcf94054ad8b93d17ec1
describe
'517632' 'info:fdaE20100110_AAACDNfileF20100110_AABOID' 'sip-files00087.jpg'
65a80b2f7aa77279eacf8c880d588706
ff8ad8614ae27b52ab6f1dd82a35a116dc717781
'2012-05-16T12:02:20-04:00'
describe
'59367' 'info:fdaE20100110_AAACDNfileF20100110_AABOIE' 'sip-files00087.pro'
b268ef093e6f56212dd8326ed7b951c3
5eb5157fe4023943405574b880d806d2d694ac0d
'2012-05-16T12:00:12-04:00'
describe
'171730' 'info:fdaE20100110_AAACDNfileF20100110_AABOIF' 'sip-files00087.QC.jpg'
d278cf7ba77c639e3b08b41a30bbb1a9
62b1fb9219781614e896b1548b4d81530739bdab
'2012-05-16T12:01:19-04:00'
describe
'3678966' 'info:fdaE20100110_AAACDNfileF20100110_AABOIG' 'sip-files00087.tif'
9e737b8ef7d5bae6ad99d1ff6580f55d
23273e06575594a526f9d1c7d46d951f089dfff5
'2012-05-16T11:58:53-04:00'
describe
'2386' 'info:fdaE20100110_AAACDNfileF20100110_AABOIH' 'sip-files00087.txt'
73970349a5b0f95e21281bf3a6442560
bfb602300bf4ad27481e322907d19563de5d2af1
'2012-05-16T11:58:00-04:00'
describe
'47928' 'info:fdaE20100110_AAACDNfileF20100110_AABOII' 'sip-files00087thm.jpg'
23fad93c7d6d023cc752183874f3cc4d
0ec0da41b34086764b78da629de178a04a6656fe
describe
'492809' 'info:fdaE20100110_AAACDNfileF20100110_AABOIJ' 'sip-files00088.jp2'
fa6c6f48edb68f316be1b75fa6a7f2b7
ccc64ded63422dbd293fd4eb6a27889c63528dc2
'2012-05-16T12:07:02-04:00'
describe
'587419' 'info:fdaE20100110_AAACDNfileF20100110_AABOIK' 'sip-files00088.jpg'
2b92ba15ec01f1249e10b4ad4d071ff3
30ea2fa08935cbe3f7b19d87eac2a5bc67407d50
describe
'282577' 'info:fdaE20100110_AAACDNfileF20100110_AABOIL' 'sip-filesi.jpg'
cc558e7c1804b2ec4b615c4b27da1130
a7f68a5419545226f3f27fb154ff0457f883d44d
'2012-05-16T12:00:04-04:00'
describe
'69318' 'info:fdaE20100110_AAACDNfileF20100110_AABOIM' 'sip-files00088.pro'
95cc9cfa98e1c432ca9d5f80969c0680
c8c4c6996ed820d457fafab3801c56d3b52dd8ac
'2012-05-16T11:57:58-04:00'
describe
'188180' 'info:fdaE20100110_AAACDNfileF20100110_AABOIN' 'sip-files00088.QC.jpg'
28b1c645f912782479e366ed30fe8dee
f39ce227345721255e25c4e77472def4155586fe
describe
'3945350' 'info:fdaE20100110_AAACDNfileF20100110_AABOIO' 'sip-files00088.tif'
f215af664d6d7634c6b0c1e6ff596a0a
2cc3f423ee33c0aa910cccdce5bb3720f0cdfbd7
'2012-05-16T11:58:03-04:00'
describe
'2726' 'info:fdaE20100110_AAACDNfileF20100110_AABOIP' 'sip-files00088.txt'
efd6baa3426e35ecca9049bf4bd6f095
17caefb1e16b63cc0003cf405bb09ca9d0211683
describe
'47951' 'info:fdaE20100110_AAACDNfileF20100110_AABOIQ' 'sip-files00088thm.jpg'
4f4496211c897b2445eda17ab471f84d
1e63c48aa254e50c877b137a5501404498d3f10d
'2012-05-16T12:02:19-04:00'
describe
'491912' 'info:fdaE20100110_AAACDNfileF20100110_AABOIR' 'sip-files00089.jp2'
b383fdba89060dbc70fc170439038711
9f17d49566be29fdc7cfeab8c4ba1cada63cead4
'2012-05-16T12:01:38-04:00'
describe
'556489' 'info:fdaE20100110_AAACDNfileF20100110_AABOIS' 'sip-files00089.jpg'
b54979ce67ae68762149d6bd9081d505
1293fc4454545bb20378748bb91db2cab6924744
describe
'64521' 'info:fdaE20100110_AAACDNfileF20100110_AABOIT' 'sip-files00089.pro'
a1f20ec7c8fbb380d3cb9532750caeae
27c887e0806d1b5acf480b5afb02195f53ba4425
describe
'176356' 'info:fdaE20100110_AAACDNfileF20100110_AABOIU' 'sip-files00089.QC.jpg'
17a7f9bb0802eb31704e342cc6544004
a8255d9abf56aa5ff58ad08ad0abcd012485c914
describe
'3937898' 'info:fdaE20100110_AAACDNfileF20100110_AABOIV' 'sip-files00089.tif'
837556566c6212c8d94ddcc1b49ba344
a1e849ded473e71b7003ab56b0d72edc42771d92
'2012-05-16T12:03:04-04:00'
describe
'2541' 'info:fdaE20100110_AAACDNfileF20100110_AABOIW' 'sip-files00089.txt'
e1fa59c644311913b39419cab7eec526
59f730a697666c1c5bd77c468af2ba64473b61e6
describe
'45839' 'info:fdaE20100110_AAACDNfileF20100110_AABOIX' 'sip-files00089thm.jpg'
5d442ea9377767f14196e1a844f94cb4
0dac83d6cab43fff3cefd32ad1328264f96299eb
describe
'494908' 'info:fdaE20100110_AAACDNfileF20100110_AABOIY' 'sip-files00090.jp2'
37628f7e7360bea295f46a3c0e90381b
23ab6002b56f704dffcaf1b2455f376b2d417571
'2012-05-16T12:00:48-04:00'
describe
'493744' 'info:fdaE20100110_AAACDNfileF20100110_AABOIZ' 'sip-files00090.jpg'
bdd94af95289c3ee53e86d2f0b2292f0
b9d6382b0ee7656278a9ad4ce714671e368d9f21
'2012-05-16T12:03:18-04:00'
describe
'68574' 'info:fdaE20100110_AAACDNfileF20100110_AABOJA' 'sip-files00090.pro'
de5b0825dd1ce77ee8886dd19d2959d5
ea5cee24930432cb89b2b04654d8b29923b4c96c
describe
'155545' 'info:fdaE20100110_AAACDNfileF20100110_AABOJB' 'sip-files00090.QC.jpg'
0614144d1d4e9364a1eefcfa8cb22cf4
adf82e9d5927131ce85846496668b97f12f7f278
describe
'3962350' 'info:fdaE20100110_AAACDNfileF20100110_AABOJC' 'sip-files00090.tif'
f28eca29b47639f2b8db244447e43c85
77f507563630c25126d4dbeb0b3c8490547de50b
describe
'3217' 'info:fdaE20100110_AAACDNfileF20100110_AABOJD' 'sip-files00090.txt'
8109dacc056f7f17f8a3a6430fab2530
7bf66fc5c36a1a155e8e194f03a3d270ba34cccb
describe
'43008' 'info:fdaE20100110_AAACDNfileF20100110_AABOJE' 'sip-files00090thm.jpg'
d4135610a70d28332aa32f90f1c5b536
3edd7b6aad7761a1f9d57dba4492b474653290ec
'2012-05-16T12:01:34-04:00'
describe
'486027' 'info:fdaE20100110_AAACDNfileF20100110_AABOJF' 'sip-files00091.jp2'
94ec282a751f0a3e408ea33e548115dc
4a56f23aec52110a182117b78ae15d559b3d956b
'2012-05-16T12:01:25-04:00'
describe
'542499' 'info:fdaE20100110_AAACDNfileF20100110_AABOJG' 'sip-files00091.jpg'
84e0d756b665fad1afe994531719e9b7
fd797309baaa35aab017245e2006b1bbd9dfc340
describe
'83309' 'info:fdaE20100110_AAACDNfileF20100110_AABOJH' 'sip-files00091.pro'
165370ec78d89fc8d5276a31d55258e7
f6a67e06fb885df130129a3eed3ae55bdef16069
describe
'168395' 'info:fdaE20100110_AAACDNfileF20100110_AABOJI' 'sip-files00091.QC.jpg'
cc585543b3ba12eb4f2ffa2fe4fb4d5f
83a2f1275645712137f2962562acbbca3ec7c202
describe
'3890758' 'info:fdaE20100110_AAACDNfileF20100110_AABOJJ' 'sip-files00091.tif'
fcf8f657a4f89c58326ed18c59fa0207
9dc1c2170d4ae16bd2f5d421491ba3e5d0caef13
'2012-05-16T12:07:04-04:00'
describe
'3918' 'info:fdaE20100110_AAACDNfileF20100110_AABOJK' 'sip-files00091.txt'
9f24b3ccaa7b67b736abffa18adae38a
d385434c54fde01c79b925d2e0331ca877715de8
'2012-05-16T11:58:08-04:00'
describe
'47515' 'info:fdaE20100110_AAACDNfileF20100110_AABOJL' 'sip-files00091thm.jpg'
bb9b889cd3ce54908395b45005f845a8
dda959f6bc9b45fd34e8ec00058700ec49373ec1
'2012-05-16T12:01:48-04:00'
describe
'496905' 'info:fdaE20100110_AAACDNfileF20100110_AABOJM' 'sip-files00092.jp2'
450795738f1272b81514ffc893b93815
0dca4f3cb1d6a939947a787b8218d3217d932b1f
'2012-05-16T12:00:11-04:00'
describe
'530235' 'info:fdaE20100110_AAACDNfileF20100110_AABOJN' 'sip-files00092.jpg'
244fd29c206eb8e0f4465b476eb23ce7
c4baf2b1c05bfbd47468724c475b8b8c774fad04
describe
'77508' 'info:fdaE20100110_AAACDNfileF20100110_AABOJO' 'sip-files00092.pro'
20635ac244010679627217df9f2e6ff0
7142cd17b251859b97a05c1aa44ef27f8d441e43
'2012-05-16T12:02:02-04:00'
describe
'167360' 'info:fdaE20100110_AAACDNfileF20100110_AABOJP' 'sip-files00092.QC.jpg'
a2a20448b1fdc9479d6870ad6dc7ef53
5f667132abedad12bda304339f3307fbdf857be4
'2012-05-16T11:59:09-04:00'
describe
'3977806' 'info:fdaE20100110_AAACDNfileF20100110_AABOJQ' 'sip-files00092.tif'
fb7c1f6b72af97330badb8a793ad00c5
73fbf016aa59b92da6bfb931f24c5c27cbd6077a
describe
'3665' 'info:fdaE20100110_AAACDNfileF20100110_AABOJR' 'sip-files00092.txt'
99ad9099d8586ef39f25985704d527e9
24364d73f1bbbfa98a7d700597c6750f2db533a2
'2012-05-16T12:06:54-04:00'
describe
'46822' 'info:fdaE20100110_AAACDNfileF20100110_AABOJS' 'sip-files00092thm.jpg'
46763198e4fab300c64ec55b7a778e6b
e42806c4036114d70f9abb640c579829033c648a
'2012-05-16T12:04:05-04:00'
describe
'492920' 'info:fdaE20100110_AAACDNfileF20100110_AABOJT' 'sip-files00093.jp2'
cea7221986f6f6c99a1fe2cffc05de3b
e1bc9aab454174d07cf68cdf8a836c8bf9d79439
describe
'510293' 'info:fdaE20100110_AAACDNfileF20100110_AABOJU' 'sip-files00093.jpg'
246fd3b218cd6875d79887664d63e93b
788f36da52b582b9b8034f63fedecd0bc30642dc
'2012-05-16T11:56:14-04:00'
describe
'69124' 'info:fdaE20100110_AAACDNfileF20100110_AABOJV' 'sip-files00093.pro'
34a98f52268ae5b71430f600fa27444f
28a9a6cce8a24d411e1bc9e6092f871a9f0bc293
'2012-05-16T12:04:58-04:00'
describe
'157482' 'info:fdaE20100110_AAACDNfileF20100110_AABOJW' 'sip-files00093.QC.jpg'
bd4ada880c9c7c9c48a76fd5640e52df
91393d4c3eafa8fb8bfd7b4f7759538cf01be301
describe
'3945842' 'info:fdaE20100110_AAACDNfileF20100110_AABOJX' 'sip-files00093.tif'
bd0a7461bda4f96ccdfe4f33b20a7428
8d2c1019e38ca806f2f91023fbb54b5e41480739
describe
'3218' 'info:fdaE20100110_AAACDNfileF20100110_AABOJY' 'sip-files00093.txt'
8b90f61fbd2872f0c3ef65b799470001
c0e776a4fb97b373c8d983152ab4f60058cb7408
describe
'44465' 'info:fdaE20100110_AAACDNfileF20100110_AABOJZ' 'sip-files00093thm.jpg'
dba6f126930bcbe4f7df728fcea7ed3c
f23a587a855a7aeaeac59b3901e2555f960e0b48
'2012-05-16T12:07:06-04:00'
describe
'495369' 'info:fdaE20100110_AAACDNfileF20100110_AABOKA' 'sip-files00094.jp2'
4e7f08f26cb0169af3d4dd9eb834f976
8a5d6cb56942f06decf508e8e28224517863ac52
'2012-05-16T12:00:14-04:00'
describe
'513970' 'info:fdaE20100110_AAACDNfileF20100110_AABOKB' 'sip-files00094.jpg'
f9531c343ecdfdc37dca6bb8b034d4ec
c7a212908d2ae634cbb343acc252bc1b9f000830
describe
'69832' 'info:fdaE20100110_AAACDNfileF20100110_AABOKC' 'sip-files00094.pro'
d66359581fa7a864f01dcbe5cdb91811
99531b293f0a2f98b52d07e360b0230d5282228d
'2012-05-16T11:57:17-04:00'
describe
'162457' 'info:fdaE20100110_AAACDNfileF20100110_AABOKD' 'sip-files00094.QC.jpg'
fddd1f60f3cd93d7d0f5df7459dc1ffd
7cfeff31aeb9b7acd4c2dd15ebeaa404a2e34770
'2012-05-16T12:04:08-04:00'
describe
'3965758' 'info:fdaE20100110_AAACDNfileF20100110_AABOKE' 'sip-files00094.tif'
35cdef1360f6afa843a298e5a3e566b9
4930adb0bfe2d0839339971c501175fa2c9c6590
'2012-05-16T11:59:45-04:00'
describe
'3286' 'info:fdaE20100110_AAACDNfileF20100110_AABOKF' 'sip-files00094.txt'
e7187ae71f6b5f7045f271a8f916533a
b7d60bc9895155ab17cab35acc76015245505520
describe
'44114' 'info:fdaE20100110_AAACDNfileF20100110_AABOKG' 'sip-files00094thm.jpg'
37438e017f4d5580b6caa02490da13ac
9c6151161a00e2fb4f22f1b4261d832d4a0ca167
describe
'480175' 'info:fdaE20100110_AAACDNfileF20100110_AABOKH' 'sip-files00095.jp2'
7edd47eecdff1f109b2355d3c502d8ea
3bd109d72f0496c59e5954d60f2b0e8fe2a67f1c
'2012-05-16T11:58:51-04:00'
describe
'514525' 'info:fdaE20100110_AAACDNfileF20100110_AABOKI' 'sip-files00095.jpg'
bfb673d4f35978c228ac6f246a6b441a
35a0df94e13c95dba5df3c06da3a39c35a6cc381
'2012-05-16T11:59:53-04:00'
describe
'74572' 'info:fdaE20100110_AAACDNfileF20100110_AABOKJ' 'sip-files00095.pro'
a08e06f263052b93d280992c25bc2014
91bf247ea84eb1e1b51f1754c9944d7132b5a678
describe
'160760' 'info:fdaE20100110_AAACDNfileF20100110_AABOKK' 'sip-files00095.QC.jpg'
4788ef5000a4b4ec06ee80996fb2467e
da05b54cfa6fe35e73fe6b41d45c8cfcce69f84d
'2012-05-16T12:02:03-04:00'
describe
'3843816' 'info:fdaE20100110_AAACDNfileF20100110_AABOKL' 'sip-files00095.tif'
4260a95a082df988d105ea810f64bb71
c4717a0601ca7f48f287e9703869d806c08ffdc8
'2012-05-16T12:02:45-04:00'
describe
'3478' 'info:fdaE20100110_AAACDNfileF20100110_AABOKM' 'sip-files00095.txt'
91137d5b8fc8055e6479211f203d66c6
eca292d1135f555ecc02520355d7fe9f19509102
describe
'48670' 'info:fdaE20100110_AAACDNfileF20100110_AABOKN' 'sip-files00095thm.jpg'
6d0395b220fb0bf38960fa90f4161a05
426f607d7c57f3965efed15e5e2a9c302df1ae1e
describe
'494004' 'info:fdaE20100110_AAACDNfileF20100110_AABOKO' 'sip-files00096.jp2'
3db3139717a1df1938ad3572e8782230
40cb1570c13b85a0f44896331d840bc459dde6fe
describe
'482607' 'info:fdaE20100110_AAACDNfileF20100110_AABOKP' 'sip-files00096.jpg'
df56eb58e1380a1159571bed03ffd6b7
e1156c36c54d20c5480258d097e56584d820bd3a
'2012-05-16T12:05:51-04:00'
describe
'64064' 'info:fdaE20100110_AAACDNfileF20100110_AABOKQ' 'sip-files00096.pro'
11d86bf085c901b1357a86a78dd0de7f
6ba27a41e9bbec305d499a5deb76a397b622c04a
describe
'148096' 'info:fdaE20100110_AAACDNfileF20100110_AABOKR' 'sip-files00096.QC.jpg'
2048a288c2e152f1a5b686d40d9ae825
5242fcdf17173365aeb2c8929574480ccf3b0e90
'2012-05-16T12:02:39-04:00'
describe
'3954392' 'info:fdaE20100110_AAACDNfileF20100110_AABOKS' 'sip-files00096.tif'
efec39fd21c86f30b25b3dffe1687121
8b4b41806dd543c23b6a77ef44e06ffdb409a775
describe
'2967' 'info:fdaE20100110_AAACDNfileF20100110_AABOKT' 'sip-files00096.txt'
3611027e7094560a9f577845bec0a0ea
5117af896110ce09be1bfc284faf1a076fb9015a
'2012-05-16T12:01:46-04:00'
describe
'40019' 'info:fdaE20100110_AAACDNfileF20100110_AABOKU' 'sip-files00096thm.jpg'
71a23f5f9ec99a2ef54b41c370a929d6
5278d52e961d58acedc48608816b3f0d29d1a225
describe
'504144' 'info:fdaE20100110_AAACDNfileF20100110_AABOKV' 'sip-files00097.jp2'
cbf9a3c691e03abd0a66d970b3eb0c7a
4ab04e83d9c87990290b3b1e008e79d1bce6debb
'2012-05-16T12:05:24-04:00'
describe
'203717' 'info:fdaE20100110_AAACDNfileF20100110_AABOKW' 'sip-files00097.jpg'
bddc6d4c5a1003e1175e4c6ff2c30339
28fc2bb809245ed4c84339f69a5f41184b424466
describe
'103419' 'info:fdaE20100110_AAACDNfileF20100110_AABOKX' 'sip-files00097.pro'
df67d1280151a3ab2535196f256f4692
04fdf194ea1a532832a6c88cca7823b9011c4a87
'2012-05-16T11:56:44-04:00'
describe
'67295' 'info:fdaE20100110_AAACDNfileF20100110_AABOKY' 'sip-files00097.QC.jpg'
7db5d8073879b141137fd7d6ced08c99
d9e14987994b803dd5eff3360570ec83aa7543db
'2012-05-16T12:00:01-04:00'
describe
'4511840' 'info:fdaE20100110_AAACDNfileF20100110_AABOKZ' 'sip-files00097.tif'
352b762225a3e7d4062f0a20a3d5d74f
3eab6543d344da4d3c16fbf4bffee2531fb37a36
'2012-05-16T11:58:55-04:00'
describe
'5940' 'info:fdaE20100110_AAACDNfileF20100110_AABOLA' 'sip-files00097.txt'
bc0619379185648ed691061c50357523
7166bc561060a7f592721b8e9b0b25e6da66a44b
describe
Invalid character
'27839' 'info:fdaE20100110_AAACDNfileF20100110_AABOLB' 'sip-files00097thm.jpg'
b665e7776cd903ca3222ac8149227f14
234ff495ca98200522a41e24034e89f329e12e70
'2012-05-16T12:06:29-04:00'
describe
'498519' 'info:fdaE20100110_AAACDNfileF20100110_AABOLC' 'sip-files00098.jp2'
48484f1503019358838ca3615ce83785
d914373bf6b58bd3deb54c0d90bbd3d98d735303
describe
'203109' 'info:fdaE20100110_AAACDNfileF20100110_AABOLD' 'sip-files00098.jpg'
85b2a0f25b888c6e186dcd2a01fb7880
e584218e45021d762628cda9958642023c799fdb
'2012-05-16T11:58:39-04:00'
describe
'93914' 'info:fdaE20100110_AAACDNfileF20100110_AABOLE' 'sip-files00098.pro'
bc12ae0f99670317cce1de088091a222
662dc2d8d71f1652cebd56bc16424af5328952ba
describe
'66703' 'info:fdaE20100110_AAACDNfileF20100110_AABOLF' 'sip-files00098.QC.jpg'
31bb76465561a04a6101b4b835935f0e
ca2e0167a81f13675ada9a08f76c63e94300a0ae
'2012-05-16T11:57:01-04:00'
describe
'4344618' 'info:fdaE20100110_AAACDNfileF20100110_AABOLG' 'sip-files00098.tif'
88b2c49ba3c0e53cd9085876743f7ac8
a484abfe53ae501db33fcd9d2ecac864119d69f9
'2012-05-16T11:59:54-04:00'
describe
'5700' 'info:fdaE20100110_AAACDNfileF20100110_AABOLH' 'sip-files00098.txt'
0ca35ff435fcc12a37c4fb62d05e464e
276e21967d3c127751774656ba1ab02f74d72047
'2012-05-16T11:56:42-04:00'
describe
'27949' 'info:fdaE20100110_AAACDNfileF20100110_AABOLI' 'sip-files00098thm.jpg'
c1a7b15430ee5772483fedb38dc9bc44
07ea58d0267ff69ee3144f372138103b51e8837c
describe
'474833' 'info:fdaE20100110_AAACDNfileF20100110_AABOLJ' 'sip-files00099.jp2'
528a6418b414ebc7e355c27bfe30e1f4
cff35557209b47c18ff689852843d72dd620f29b
'2012-05-16T11:57:42-04:00'
describe
'425893' 'info:fdaE20100110_AAACDNfileF20100110_AABOLK' 'sip-files00099.jpg'
3443bd3ea37482efa4757e46487d4aaf
c517ea33c4a48ad783a620a576ae1ac72bf3dd4b
describe
'43698' 'info:fdaE20100110_AAACDNfileF20100110_AABOLL' 'sip-files00099.pro'
94499ec1daac66f527b6d775212e78d3
29b7aaebcfb27e470198486008600a30f74d8071
describe
'127044' 'info:fdaE20100110_AAACDNfileF20100110_AABOLM' 'sip-files00099.QC.jpg'
92a0d439de3bc332c8f2aa2474ba5796
22fc16d773e2dbffcf95b8c0c23ac76c4c4d2f2f
'2012-05-16T12:05:52-04:00'
describe
'3801458' 'info:fdaE20100110_AAACDNfileF20100110_AABOLN' 'sip-files00099.tif'
5eef06f4c201f64f6ffa619f37f77048
45494f64974ddf963fed0bcf56d11ff358147371
describe
'1999' 'info:fdaE20100110_AAACDNfileF20100110_AABOLO' 'sip-files00099.txt'
fda7b8660d654028026f8a5a98538364
34413c2d598842d4d89354e55b18446a74a277cc
'2012-05-16T12:04:13-04:00'
describe
'35056' 'info:fdaE20100110_AAACDNfileF20100110_AABOLP' 'sip-files00099thm.jpg'
63130e57e99c66d9be0bd7b3d960e5b6
ef749aa4a638b3790c01b485536225cb21fdb550
describe
'494129' 'info:fdaE20100110_AAACDNfileF20100110_AABOLQ' 'sip-files00100.jp2'
331e7f095cd30a450398303ccf9eb970
02f21f519bfff881cc52c00586a284e13ef2ba6b
'2012-05-16T11:56:22-04:00'
describe
'164888' 'info:fdaE20100110_AAACDNfileF20100110_AABOLR' 'sip-files00100.jpg'
aba86e6edd521e8626331c22f368de99
978329bd6c58aaf3baf9fffd20ad18051e26a9be
describe
'17099' 'info:fdaE20100110_AAACDNfileF20100110_AABOLS' 'sip-files00100.pro'
cbb8e33d7e2d72f68f2069168c46c7dd
b94aa6ac57312f789208f3d4bc10e1e884ffc1b2
describe
'56266' 'info:fdaE20100110_AAACDNfileF20100110_AABOLT' 'sip-files00100.QC.jpg'
a598cfe8742582838e04c0e82ad67b4c
44c93a74824b6deff497f1574c0964551c87fb98
describe
'4051600' 'info:fdaE20100110_AAACDNfileF20100110_AABOLU' 'sip-files00100.tif'
d595a842dc7033598a845a87e609f167
126313f99e0ca0483bd7688ec340443bf7237ffc
'2012-05-16T11:57:39-04:00'
describe
'976' 'info:fdaE20100110_AAACDNfileF20100110_AABOLV' 'sip-files00100.txt'
0a638707241481d43aaab8f792b2751c
2848b10c169e81d128a7af0ca681635651665fa2
describe
Invalid character
'25491' 'info:fdaE20100110_AAACDNfileF20100110_AABOLW' 'sip-files00100thm.jpg'
25e6d9ca5890f70f23aa52616e32382e
6b48fa01f29bcb6077276225d23e42c8306fc7aa
'2012-05-16T11:58:16-04:00'
describe
'485647' 'info:fdaE20100110_AAACDNfileF20100110_AABOLX' 'sip-files00101.jp2'
132e94943000f8ad16c1df0e83a58f96
2487ca280541497f080fe96e56ad137f0efb9732
describe
'138587' 'info:fdaE20100110_AAACDNfileF20100110_AABOLY' 'sip-files00101.jpg'
4b8fc1f3b3c62cc3955ff0428110f3c2
6bf76ac4522db9c8e9e758d2bc4da47189815ca5
'2012-05-16T11:57:47-04:00'
describe
'10070' 'info:fdaE20100110_AAACDNfileF20100110_AABOLZ' 'sip-files00101.pro'
187b5114b3b383d641e223afc39ed6b3
17f43f50b37922dfa206d44a10dd35a682414590
describe
'48301' 'info:fdaE20100110_AAACDNfileF20100110_AABOMA' 'sip-files00101.QC.jpg'
a1a8e4ed0f0ea3eb4583a4d9bd4c60e3
2dbf1f7e0d1fcab7c574dd9a2d653c4013682781
describe
'3807152' 'info:fdaE20100110_AAACDNfileF20100110_AABOMB' 'sip-files00101.tif'
894dbeb3189cfb354ae9f00bc0134176
cc8d89f969dbf91ff7838fddb963aabf0150861e
describe
'609' 'info:fdaE20100110_AAACDNfileF20100110_AABOMC' 'sip-files00101.txt'
4583f8c7b8b88a724321de30b3facf7b
f5bdbf776d2c95c3b0cb126d1d5b09ed8b54b689
'2012-05-16T12:05:53-04:00'
describe
'22299' 'info:fdaE20100110_AAACDNfileF20100110_AABOMD' 'sip-files00101thm.jpg'
2fbd38b631838a8079be3552b489c1fd
fcc2edf4a385da102de704e2b931a2798693b2d9
'2012-05-16T11:56:20-04:00'
describe
'8390' 'info:fdaE20100110_AAACDNfileF20100110_AABOME' 'sip-filesi.pro'
3cfc772de7d24fc55d5e0a177d03265e
535c503f6f38823ee384c387ae2175c417a1411e
'2012-05-16T11:58:01-04:00'
describe
'85446' 'info:fdaE20100110_AAACDNfileF20100110_AABOMF' 'sip-filesi.QC.jpg'
914af9c61ab07773a5e7f66ee584f068
6cea70d5de21e97f47976d4e69ea8ac54def05a3
'2012-05-16T12:01:20-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABOMG' 'sip-filesi.tif'
5c4ccbe561211bd22516d204832885d9
8d27b45b2648a6f70c46d1c6dc65505c538f5711
'2012-05-16T12:06:12-04:00'
describe
'501' 'info:fdaE20100110_AAACDNfileF20100110_AABOMH' 'sip-filesi.txt'
76d9fb1b2148a6ce025ccd80aab6839c
c22c66b0f0df355e66dc4f45c57c1460a9def0f9
describe
'2290324' 'info:fdaE20100110_AAACDNfileF20100110_AABOMI' 'sip-filesii.jp2'
1544a604ff3e2be9cb38c8dd597cae97
85f93f128e916e870fe1ce7f0d324c5218fdb293
describe
'510221' 'info:fdaE20100110_AAACDNfileF20100110_AABOMJ' 'sip-filesii.jpg'
6ee3c1d9838392a31b27e314c7bc5564
8057e4cb60ddaab9179d6f0ec3291ce32ec3a9cf
'2012-05-16T12:04:39-04:00'
describe
'5930' 'info:fdaE20100110_AAACDNfileF20100110_AABOMK' 'sip-filesii.pro'
97e57cd3cc94fb0344c1d20528f4dca8
fdccccb58426dc655ddf6e49d0b231d79edbdf96
describe
'136616' 'info:fdaE20100110_AAACDNfileF20100110_AABOML' 'sip-filesii.QC.jpg'
aded0f3d800c30b9deae3713e273254a
3354f7db21c12449037ab1b3dce8d56fc9ecaa30
describe
'18328444' 'info:fdaE20100110_AAACDNfileF20100110_AABOMM' 'sip-filesii.tif'
48a5b3e33531ef9bdf74a45d237de761
855dc08b8d82cf95f8355238ca8bc5f456ba5407
'2012-05-16T11:56:04-04:00'
describe
'304' 'info:fdaE20100110_AAACDNfileF20100110_AABOMN' 'sip-filesii.txt'
db945ba25c1d897175d07181ae846c9c
5407bdf9c527617269d2ae6b84ee693f59cca10b
describe
'461941' 'info:fdaE20100110_AAACDNfileF20100110_AABOMO' 'sip-filesiii.jp2'
896563ac9a8b4c8da93e9348ffb24906
5d8891bfa5ab3eaced658b09ff0ac572d468b379
'2012-05-16T12:06:15-04:00'
describe
'570281' 'info:fdaE20100110_AAACDNfileF20100110_AABOMP' 'sip-filesiii.jpg'
9789726b5b642bb58b48d6308eb1cacb
969cdc180ad03045afff8f2e8cdfa8a2dc96aa6d
'2012-05-16T11:59:20-04:00'
describe
'65001' 'info:fdaE20100110_AAACDNfileF20100110_AABOMQ' 'sip-filesiii.pro'
743fb25400638a1e4d16cc8584c9328f
3d920f4cd21bfe3db0c6db9c68d0fce0b60de23b
'2012-05-16T12:01:45-04:00'
describe
'info:fdaE20100110_AAACDNfileF20100110_AABOMR' 'sip-filesiii.QC.jpg'
31ab54012c8a692dee1a7c902b8cba89
c0be91a8b5372b0977ab306b216b1b97a525f797
'2012-05-16T11:56:23-04:00'
describe
'3697932' 'info:fdaE20100110_AAACDNfileF20100110_AABOMS' 'sip-filesiii.tif'
66608949eac778a006a2397e5400a976
b62d2246dce606473346d2699a0cede7b5f3124c
'2012-05-16T11:56:02-04:00'
describe
'2593' 'info:fdaE20100110_AAACDNfileF20100110_AABOMT' 'sip-filesiii.txt'
8af7d7c28e670226c5a58e73deb9af9c
157c4d948b02ecc7437396f50cf76f72b7cc0663
describe
'50591' 'info:fdaE20100110_AAACDNfileF20100110_AABOMU' 'sip-filesiiithm.jpg'
0aab757b09bd3be53d21a34e1551974e
37dca0dfcb96f786b0f64bd440e97bc088fd1d19
describe
'37551' 'info:fdaE20100110_AAACDNfileF20100110_AABOMV' 'sip-filesiithm.jpg'
1e302474ee6ab09e48ccdcc610a0f6c0
95f48cbf2db0897abd241997c439a004493d4ade
describe
'25068' 'info:fdaE20100110_AAACDNfileF20100110_AABOMW' 'sip-filesithm.jpg'
1665dd95768d74597be405cfa9d9c39a
75f9a9350fb952fdaac77a7e8259a9ecfd313583
'2012-05-16T11:59:16-04:00'
describe
'453570' 'info:fdaE20100110_AAACDNfileF20100110_AABOMX' 'sip-filesiv.jp2'
5856b05b1c6b16f7033da547bce1bfec
b0ccefbfda5c4b972775d296b00488b278f87902
describe
'293210' 'info:fdaE20100110_AAACDNfileF20100110_AABOMY' 'sip-filesiv.jpg'
8845814b334d81d81ad9cb0ad1b112c4
bc7687e7a8a50f21db6018ff32358edc616777b0
describe
'8509' 'info:fdaE20100110_AAACDNfileF20100110_AABOMZ' 'sip-filesiv.pro'
2d363052ff793fe594629a52419c9a78
56c9010e24f9bbf88571c83fd6289f49b8233dbf
'2012-05-16T11:56:39-04:00'
describe
'86683' 'info:fdaE20100110_AAACDNfileF20100110_AABONA' 'sip-filesiv.QC.jpg'
4b83a9b73aa8adfd314b8cdfdc53f4d1
5f858ac6e8ed583311c0686c794848c6228b2ef0
describe
'3631954' 'info:fdaE20100110_AAACDNfileF20100110_AABONB' 'sip-filesiv.tif'
afed9c26f541e0306013c7c9c8a1e423
a72cf95d69a9e52b545cd98d6fb4d0d985cbf4a0
'2012-05-16T12:02:16-04:00'
describe
'426' 'info:fdaE20100110_AAACDNfileF20100110_AABONC' 'sip-filesiv.txt'
eeba86673e2a88c688e3904898e4d559
db11001395ee7194b09c74ba6e53f991acc4d853
describe
'24893' 'info:fdaE20100110_AAACDNfileF20100110_AABOND' 'sip-filesivthm.jpg'
166cbc5badc158761ce5a7c56c4521f5
22a3ed948b174cddc446c8fa1672e7728891430e
'2012-05-16T12:04:56-04:00'
describe
'463607' 'info:fdaE20100110_AAACDNfileF20100110_AABONE' 'sip-filesix.jp2'
a6adf1f9dab0d9cdb853d7554780208d
e06846f9118444e722cf767776a3186b625ce1f4
'2012-05-16T12:03:19-04:00'
describe
'405443' 'info:fdaE20100110_AAACDNfileF20100110_AABONF' 'sip-filesix.jpg'
c3d9c5c5fc7dde5afab83b1cf63aaf22
7e21ad93bdf01ad0389b830afebdec9518f9b28d
describe
'64516' 'info:fdaE20100110_AAACDNfileF20100110_AABONG' 'sip-filesix.pro'
0637e3fc2b0cb43c1a071ac5e94a2b75
04cd6c70c91657a35dcbfc11ac2eb64ddce2707c
describe
'120517' 'info:fdaE20100110_AAACDNfileF20100110_AABONH' 'sip-filesix.QC.jpg'
b6b16ea04dd806806c37cab2615b04a3
8ff3aa9aa8cb4be57b19a585c3991411b46788ea
describe
'3711226' 'info:fdaE20100110_AAACDNfileF20100110_AABONI' 'sip-filesix.tif'
ffc28a6887d7caa586655fad5b5be6c2
4afe016ea9ab63f359731d2ef28982251ce6fbd9
'2012-05-16T11:58:25-04:00'
describe
'3064' 'info:fdaE20100110_AAACDNfileF20100110_AABONJ' 'sip-filesix.txt'
41d35b2a859febac70c6b5181600c5c4
0ff4e31dd31731aa5f7c152d7d4efb3dadbea449
describe
Invalid character
'34461' 'info:fdaE20100110_AAACDNfileF20100110_AABONK' 'sip-filesixthm.jpg'
93f205d9eff55b514eaf747070d0d307
20a79dda1602b87e82ce7b3332bd57a951f1d873
describe
'134408' 'info:fdaE20100110_AAACDNfileF20100110_AABONL' 'sip-filesUF00000242_00001.mets'
e2c349664ffe4b4e1081215cae9c533b
6e475c1ec2d7c6738a314d337e3e94730eeb853b
describe
TargetNamespace.1: Expecting namespace 'http://www.uflib.ufl.edu/digital/metadata/ufdc2/', but the target namespace of the schema document is 'http://digital.uflib.ufl.edu/metadata/ufdc2/'.
'2015-10-09T09:55:53-04:00' 'mixed'
xml resolution
http://www.uflib.ufl.edu/digital/metadata/ufdc2/ufdc2.xsd
BROKEN_LINK schema http://www.uflib.ufl.edu/digital/metadata/ufdc2/ufdc2.xsd
The element type "div" must be terminated by the matching end-tag "