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A geologic guide to the Suwannee River, Ichetucknee Springs, O'Leno, and Manatee Springs State Parks ( FGS: Leaflet 12 )

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Title:
A geologic guide to the Suwannee River, Ichetucknee Springs, O'Leno, and Manatee Springs State Parks ( FGS: Leaflet 12 )
Series Title:
Leaflet
Creator:
Hoenstine, Ronald W.
Weissinger, Sheila.
Place of Publication:
[Tallahassee Fla.]
Publisher:
Bureau of Geology, Division of Resource Management, Florida Dept. of Natural Resources
Publication Date:
Language:
English
Physical Description:
28 p. : ill., maps ; 23 cm.

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Subjects / Keywords:
Geology -- Florida. ( lcsh )
Parks -- Florida ( lcsh )
Suwannee River, FL ( flgeo )
Ichetucknee Springs ( flgeo )
Limestones ( jstor )
Rivers ( jstor )
Natural springs ( jstor )

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University of Florida
Holding Location:
University of Florida
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The author dedicated the work to the public domain by waiving all of his or her rights to the work worldwide under copyright law and all related or neighboring legal rights he or she had in the work, to the extent allowable by law.
Resource Identifier:
AAA2599 ( NOTIS )

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Full Text
Leaflet No. 12
Page
Introduction ........................................... 1
Suwannee River State Park ....................... 7
Ichetucknee Springs State Park ............... 13
O'Leno State Park .................................. 19
Manatee Springs State Park ...................... 25
On the cover: Limestone outcrop at S uwannee River State Park
Prepared by
Bureau of Geology
Division of Resource Management
Florida Department of Natural Resources 1982




A GEOLOGIC GUIDE
TO SUWANNEE RIVER,
ICHETUCKNEE SPRINGS, O'LENO,
AND MANATEE SPRINGS STATE PARKS
by
Ronald Hoenstine and Sheila Weissinger
INTRODUCTION
Much of North Central Florida is sparsely populated and retains the nearly-untouched beauty of "Original Natural Florida," the Florida that greeted the early European explorers. Located in this area of scenic rivers and sparkling springs are several popular state parks, including Ichetucknee Springs, Manatee Springs, O'Leno and Suwannee River.
GENERAL TOPOGRAPHY
Much of the area's distinctive beauty is associated with small and large solution depressions, springs, and disappearing rivers; topographic features representative of a general
landform designated as "karst" by geologists. These features develop in limestone regions having plentiful rainfall. Sinkholes are numerous in the area, and are conspicuous
features in the parks.
SINKS
Sinks occur as a result of the dissolution of limestone by the downward percolation of rain water. Rain combines with carbon dioxide in the atmosphere to form carbonic acid. As this aciI




dic rain percolates downward through the soils it comes into contact and reacts with the underlying limestone. The result. is dissolution of the limestone and the formation of cavities. As the cavities grow with time, the weight of the overlying sediments may cause collapse and the subsequent formation of a sinkhole. This process of formation may become accelerated in the future if this pristine area of Florida is subjected to increased amounts of acid rain.
Some of these sinkholes are filled with water, while others are "dry sinks." While both groups of sinkholes may have continuity with the underlying limestone, the dry sinks permit rain water to percolate completely into the underlying limestone.
SPRINGS
Also associated with this karst terrain are numerous spri ngs. Fl ori da has 1 ong been famous for its springs. In fact, there are more large springs in Florida than any other-state, accounting for 27 of the nation's 78 major springs. It
has been calculated that the total output of water from all of Florida's 300 known springs is around 8 billion gallons a day.
To more fully appreciate how and why springs form, one must understand the term
*aquifer." Hydrologists define aquifers as natural zones below the ground surface that
yield water in quantities that are important economically. In this part of Florida the aquifer, which is known as the Floridan Aquifer, is a thick layer of limestone. This limestone is divided into formal units called formations. These formations, which vary in age and lithology (physical characteristics), include the Suwannee Limestone and limestone of the Ocala Group.
Rocks must have two essential properties to




be considered an aquifer. They must have porosity and permeability." Porosity refers to the openings in the rocks which have the capacity to store water. Such openi ngs i ncl ude cavi ti es, voids or intergranular spaces. The second property, permeability, is equally important as it refers to the rocks' ability to transmit water through interconnected pore spaces.
Although highly variable, parts of the
Floridan Aquifer may contain as much as 30 percent open space capable of storing large quantities of water. Furthermore, the aquifer's permeability permits the movement of vast quantities of water to the surface via springs and wells.
A spring occurs when groundwater from the aquifer is discharged as natural seepage or freeflow through an opening at the ground surface. The volume of water discharged may be small and form a trickle, or large enough to form a river, such as the Ichetucknee River. The volume discharged frequently varies, as it is dependent not only on porosity and permeability but other factors such as seasonal rainfall that recharges the aquifer, and pumpage, which depletes it.
AGE OF THE GEOLOGIC FEATURES
An age (time of deposition) of about 30 million years before the present, during a period of time known as the Oligocene Epoch, can be assigned to the limestone and dolomite which crop out in the Suwannee River State Park. An age of about 40 million years before the present (Late Eocene Epoch) can be assigned to the limestone occurring at the surface in the vicinity of Manatee Springs, Ichetucknee and O'Leno state parks.
How do geologists determine the age of these rocks? A casual glance at the limestone
3




exposed in these parks reveals the -presence of marine fossils such as clams and.oysters,- while a closer microscopic inspection reveals numerous microfossils. Microfossils are the remains- of tiny plants and animals that- lived long ago. These organisms include, among others, the silicabearing plants called diatoms, calcareous marine algae known as coccoliths, and calcareous one-celled animals known as foraminifera. The presence of microfossils in rocks serves as an important tool for various scientific groups, such as the Florida Bureau of Geology, in providing data for the dating of Florida's sedimentary rocks.
Essential to the study of microfossils is the accepted principle that various species of plants and animals lived and died during certain periods of Earth's history. Therefore, the identification of these species, together with a knowledge of their life span, permits one to date the sediments in which they are found.
ANCIENT ENVIRONMENTS
Microfossils' small size, wide geographic occurrence, and abundance in sediments of all ages and diverse environments are characteristics that make them invaluable for the purpose of identifying ancient depositional enviroments. Specifically, microfossils can be important indicators of the water depths, temperature, salinity, and water currents that existed at the time the sediments were formed. For this reason, the utilization of microfossils has been of special importance in the study of Florida's past and in identifying the depositional environments that existed in the-area of the four parks 30 to 40 million years ago.
By comparing these microfossils with living relatives, we know that the sediments present in
these parks were formed in a relatively shallow
4




marine environment. In-other words, the limestone you see in the parks was once covered by a shallow -sea. The period of time when the Florida peninsula was underwater represents most
of the last 200 million years of geologic history.
The importance of microfossils to the study
of Florida's past can be further illustrated by comparing the past environment of Florida to that of much of the rest of North America during the Cretaceous, a period of time that ended approximately 65 million years ago. During this period, when dinosaurs roamed much of North America, these parks, and indeed most of Florida, were underwater. This explains the
absence of dinosaur remains in Florida.
We hope this geologic guide will serve to enhance your enjoyment and appreciation of the beautiful and distinctive state parks of the Suwannee River Basin.




U N RIV
C, Af a M to...... .
0m me
06
Ear hwr l SUWANNE RIVER
STAT E PARK
0 100 9 tac Feetntrr~




SUWANNEE RIVER STATE -PARK
INTRODUCTION
The confluence of the Withlachoochee and Suwannee rivers offers a unique and historic setting for the Suwannee River State Park. Visitors to the .,park are impressed with the quiet natural beauty of the rivers and the surrounding wooded uplands, Situated in the physiographic zone known as' the Coastal Lowlands, the park's elevation ranges from a low of 40 feet above MSL (mean sea level) near the river to a maximum of 70 feet MSL near the eastern boundary of the park.
THE RIVERS
Originating in the Okefenokee Swamp of southeast Georgia, the Suwannee River winds through north central Florida past the park, continuing its journey to the Gulf of Mexico, its final destination. Similarly, the Withlacoochee River originates in south Georgia and flows southward to merge with the Suwannee River
at the park, where this confluence of the two rivers can be viewed from a rustic overlook (see map). The distinct differences in sediment loads of the rivers can be observed from this vantage point. The light brown waters of the Withlacoochee are laden with suspended silts and
clays which give the river a muddy appearance. In contrast, the Suwannee River is relatively free of suspended sediment. Its dark, brownishblack color is a result of high tannic acid content. This tannic acid is produced by decayed
7.




View of Suwannee River
T
Tlihe Confluence of the Withiacoochee and Suwannee rivers.




organic matter which washes into the river from forests and swamps that line the shore.
As the rivers flow southward they wind, or meander, resulting in rock and soil material being eroded from the outside and downstream side of river bends, while material is deposited on the inside and upstream side. You can observe this effect as you hike along the river trail.
LIMESTONE EXPOSURES
The effects of river erosion are evident in
the park. As you walk southward along the river towards the earthworks and the overlook or
northward along the river side of the Suwannee RiVer Trail, you can observe limestone and dolomite outcrops on the south side of the river. The river has eroded the overlying sediments to expose these aged and weathered rocks.
These limestones, which are part of the Suwannee Limestone, were deposited during Oligocene time (30 million years before the present). Through time, much of the limestone has experienced substantial dol omi ti zati on. This process occurs when limestone, composed of the nineral calcite (a calcium carbonate), becomes a different mineral, dolomite, through the substitution of magnesium for calcium. As a result the rock, which in its original state was porous and permeable, may become dense and impermeable. In addition, fossils usually become distorted or completely obliterated through this process of dolomitization. A close examination will reveal fossil shells, molds and worm borings exhibiting all degrees of preservation. West of the overlook is a prominent
9




exposure of dolomite and limestone which, depending on the river stage, can measure more than 15 feet in height.
SUWANNEE RIVER TRAIL
Walking along the Suwannee River Trail one can not only observe limestone outcrops but also
see low banks parallel to the river on the eastern side of the trail (see map). These low ridges, called natural levees, are formed as a result of the river flooding. As the river overflows its banks, an abrupt decrease in both water velocity and turbulence occurs, resulting in the deposit of the coarser particles of the suspended sediments. In time, these coarse deposits form ridges, or levees, which generally
parallel the river's edge.
SANDHILLS TRAIL
The Sandhills Trail leads from the hardwood hammock along the river to the open forest of pines. Approximately 500 feet down the trail one can see several dry sinks on the northeast side (see map). These geological features, which have a diameter of approximately 20 feet and a depth of 10 feet, are collapsed limestone cavities (see "sinks", page 2).
The trail continues to the Old Columbus Cemetery. The town of Columbus has long since disappeared, but some of its history remains on the weathered tombstones. One can see the
results of weathering (especially the corrosive action of rain) on both the metal and stone markers. The once clearly legible monuments are now smooth due to the effects of rain and abra10




sion from wind-blown sediments over a relatively short period of time. Imagine the effects of weathering on Florida's landscape over a period of millions of years.
Dry sink along Sand Hills Trail
11




chs.ok e l. to ,
;h38 Area Stto ICHETUCKNEE SPRINGS Tb n ao
A Hole Blue Hole STATE PARK Access Trail ~ Trestle Point
Noture
TrollI
0 2000
feet




..ICHETUCKNEE SPRINGS STATE PARK
INTRODUCTION
South of Suwannee River State Park, strad.dling the Suwannee-Columbia county line, .is Ichetucknee Spri ngs State Park, one of the most beautiful and popular parks in Florida. For many people its refreshing springs represent a cool oasis during the hot summer months. Elevations range from 25 feet MSL near the river to a maximum of 60 feet -MSL in the western part of the park.
The surrounding area has many features typical of a karst area. These include wet and dry sinks and numerous springs.
THE SPRINGS
Within the 2,241 acres that make up the park and along the upper reaches of the Ichetucknee River are nine named and many unnamed springs. The most northern spring is Ichetucknee Spring which forms the headwaters of the river. Nearby is Blue Hole Spring, which can be reached by a trail and boardwalk from the main park.
Ichetucknee Spring is 75 feet wide and 105 feet long, and has a maximum depth of 14 feet. The spring has an average water temperature of 730F and discharges 30 million gallons of water a day (based on measurements taken in 1975 by the U.S. Geological Survey).
The trail just north of Ichetucknee Springs
leads to Blue Hole (Jug) Spring (see map). This secluded spring with its crystal clear, blue
13-




waters is a favorite swimming site in the park. The spring is 85 feet wide, 125 feet long, and has a maximum depth of 37 feet at its north central end near the vent. The boil, which is clearly visible near the center of the pool, has a measured flow of 60 million gallons a day.
View of Ichetucknee Spring and spring run
14




LIMESTONE
The spring's waters issue directly from the limestone aquifer. The exposed limestone which forms part of the aquifer in this park is the Ocala Group limestone of Eocene age. These limestones, which are approximately 40 million years old, contrast with rocks cropping out in the Suwannee River State Park in that the exposed limestones there are the Suwannee Limestone of Oligocene age (approximately 30 million
years before the present). Thus, as we have come southward, we have taken a 10 to 15 million year journey back in time. The missing, younger, Suwannee Limestone, which would ordinarily overlie the Ocala limestones, was either never deposited here or was completely eroded over time.
Limestone outcrop along Blue Hole Access Trail
15




These limestones offer further contrast to those in Suwannee River State Park in that little dolomitization can be observed here. Because these rocks are primarily limestone (calcium carbonate), the fossils show better preservation. However, the calcium carbonate content of these rocks causes them to be more susceptible to dissolution by acidic rain. Similiar to the limestone exposed at Suwannee River State Park, these limestones, though much older, also once formed the bottom of an ancient, shallow sea.
TRESTLE POINT NATURE TRAIL
A walk along the clearly marked Trestle Point Nature Trail leads the visitor through hardwoods and pines that line the river (see map). Limestone outcrops of the Ocala Group can be seen along this trail at the river's edge. Directly across from Trestle Point you can see a tunnel formed by dissolution of the limestone. Other dissolution features observed along the river bank include cavities and irregular voids, many of which resemble caves and columns. These surface structures are very similar to features occurring in the limestone subsurface.
Farther down the trail you can see a large, circular depression approximately 60 feet to the left of the trail. This depression is a dry sink which formed through dissolution of the underlying limestone by rain water. Several additional sinks similar to this one can be observed within the park boundaries.
16




Continuing along the trail you will come to an overlook. This overlook permits you to see the remnants of an old hard rock phosphate mine which was being actively mined in the early 1900's. Note the trees' position and orientation with respect to the sloping sides. The distortion in their growing position is due to a process known as "soil creep." This process
occurs as a result of gravity causing the slow, downhill movement of poorly-consolidated sediments, such as sands, that are present here. This movement, though very slow, has noticeable effects over time.
The closest active phosphate mining today occurs in Hamilton County at a site approximately 40 miles north of the park. Phosphate represents one of Florida's greatest mineral resources and production in Florida exceeds that of any other state.
k -.
Soil bank erosional features at Trestle Point
17




o 500
feet
Co ~~Picnic $ 2b Entrance~o-" ., b Area w ~Static
Bridgecamp o 'LENO
STATE PARK iver




O'LENO STATE PARK
INTRODUCTION
A short drive south- from Ichetucknee
Spri ngs State Park brings you to O'Leno State Park, located on the peaceful Santa Fe River. This interesting, scenic park has a general topography much like that of Ichetucknee, with numerous wet and dry sinks and limestone exposures. Elevations within its boundaries vary from a low of about 40 feet MSL to a maximum of approximately 79 feet MSL at the park's northwestern border.
THE RIVER
The Santa Fe River is fed by many springs and tributaries, including the Ichetucknee River, which joins the Santa Fe after a brief 5-1/2 mile journey from its headwaters. In contrast to the crystal clear Ichetucknee River, the waters of the Santa Fe are stained dark by tannic acid. The river's surface reflects like a mirror the luxuriant vegetation along the shore.
19,




A suspension bridge, built in the 1930's by the Civilian Conservation Corps, spans the river at the main park (see map). Below it is a small rapid, created when local dolomitic limestones were placed there as part of the construction of a mill that once stood on this site. Many limestone outcrops occur along the river and park trails.
The suspension bridge spanning the Santa Fe River.
20




THE LIMESTONE TRAIL
Located to the left just past the park's entrance is the Limestone Trail (see map). This forest trail, which can be traveled in a leisurely 20-minute walk, presents the opportunity to observe numerous limestone boulders and are approximately 40 million years old, about the same age as those found in Ichetucknee Springs State Park to the north. In addition, one can observe an abandoned limestone quarry at the trail's overlook located on the northeastern side of the trail. Note the prominent limestone
outcrop clearly visible at the south end of the quarry. Large quantities of limestone were
mined from this now-inactive quarry for use in the construction of fireplace chimneys.
As you continue your walk, you will see a large sinkhole to your left on the western side of the trail.
21




RIVER NATURE TRAIL
From the main park and just across the suspension bridge, one comes to the River Nature Trail (see map). This picturesque trail leads through lowland hardwoods and sandy pine forests
within the river's flood plain. Several features of geologic interest can be observed along the way.
Approximately 1,500 feet down the trail is a long, narrow lake. The water in this lake, which has direct access to the aquifer, fluctuates in response to groundwater levels.
View of lake located on north side of River Nature Trail (water level responds
directly to fluctuations in underlying aquifer).
22




The next geologic feature of interest is the River Sink, which is located at the eastern end of the trail. It is here, observable from several vantage points, that the Santa Fe River disappears and flows underground for more than 3 miles before it again becomes a surface stream. The waters of the river are literally "swallowed up" by vertical, 100 foot deep conduits. These conduits channel the water downward into the subsurface limestones where the water travels laterally for several miles through cavities before reappearing at the surface. Such a phenomenon, creating what is known as a natural bridge, is not unusual in these regions of springs and sinks.
As you leave River Sink you can see on the southern side of the trail, a large, shallow depression. Clearly marked with a park sign, this depression is a dry sink.
River Sink
23




STATION
N Boys,
Camp
MANATEE FGirls'
SPMANTEE Camp MANATEE SPRINGS
sinST E Large
we? STATE PARK
|~ 3wet sinks




.MANATEE SPRINGSSTATE PARK
INTRODUCTION
Manatee Springs- is situated in a lush, semitropical, hardwood hammock just 23 miles northeast of the Gulf of Meico. In addition to providing many recreational activities, the park contains excellent: examples of karst landforms.
The park is located in the physiographic zone known as the Coastal Lowlands, with elevations ranging from a low of near mean sea level at the river to a high of 25 feet above MSL in the park's interior. The area is rich in history, for these springs were known and visited for centuries by the Indians and early Spanish explorers. Today, thousands of tourists come to enjoy the sparkling, -clear waters and tranquil surroundings. In the winter its namesake,- the endangered Florida manatee, sometimes visits the springs to enjoy its constant 720F temperature.
THE SPRINGS
The spring head, which is located 1,200 feet from the Suwannee River, discharges 4.8 million gallons of water per hour. The water issues from rock which is part of the Ocala Group--limestone, the same limestone formation that is found in O'Leno and Ichetucknee Springs state parks to the north. These rocks, which can be observed -as .outcrops around' the pool 's perimeter, are approximately 40 .million years old.
An excellent view of the spring run can be
25 -




enjoyed from a boardwalk that leads from the boat launching area to the Suwannee River. Much of what may be seen as you walk along this boardwalk is similar to what was reported by William Bartram, a naturalist, in his visit to the spring in 1774. On this visit, he observed alligators, gar, catfish, mullet, trout, bream, pike and "the monstrous amphabious maneta (manatee)". He also noted great quantities of shells and shell fragments in and around the spring.
A large underwater cave system extends 2,000 feet from the main spring. Scuba diving in these caves is very popular, but dangerous, and safety is emphasized by park personnel.
View of the boil and spring run
26




NATURE (SINK) TRAIL
The Nature Trail begins at a point approximately one mile from the entrance station, just east of the camping area. This clearly marked trail leaves the main road and winds through a dense hardwood hammock toward the southeast. Visible on both sides of the trail are depressions, or sinks, of varying sizes and stages
of development. Of particular interest is a series of three wet sinks located near the trail 's end. Two of the sinks are connected by a narrow landbridge. This connecting bridge is underlain by rocks which have not experienced dissolution and subsequent collapse. In the
future, the adjoining sinks may enlarge, engulfing the bridge.
Two much larger sinks can be observed in the nearby camping area (see map). -These sinks, which are filled with water, are connected via a network of underground solution channels to the main springs.
11Z
Information markers throughout the parks provide visitors with trail guides
and descriptions of special features.
27




Two of the sinks are connected by a narrow landbridge. This connecting bridge is underlain
by rocks which have not experienced dissolution and subsequent collapse. In the future, the adjoining sinks may enlarge, engulfing the bridge.
One of several wet sinks located along the Sink Trail.
28




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PRO28 11577a3adb9b0366a7a2db0fcf37f377 28144
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TXT1 textplain 8d8bae44a462ad1f50372ef7870402dd 476
00001.txt
TXT2 6cad5a4cb9162c9e07a5a46e25d5ccb3 1119
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TXT3 2e9efd14b72f35299ef68b1eb0a54e34 1691
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TXT4 75ad680f908daea84ef2a25d0aec30f1 1666
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TXT5 a44204e732c9bd4e8e01389d1878b9bc 1755
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TXT6 02b93f1713f853f751d07a6297e0f1b5 852
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TXT8 58ce6d741f0888d855349714fe1dab68 1366
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TXT20 c11b6efb323467b1b1c464a5a50f5077 850
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TXT26 11f1b2d07322446332818bb381fcc237 1324
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TXT27 d213e3c794c56271cbc8968f5eab21e1 690
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PDF1 applicationpdf 237027e694db2f8bcfbdb1b6f7be7d39 1568782
UF00001180.pdf
METS2 unknownx-mets 2186f6012d63574112403e452c5eec89 34991
UF00001180_00001.mets
METS:structMap STRUCT1 physical
METS:div DMDID ADMID A ORDER 0 main
PDIV1 1 Title Page
PAGE1
METS:fptr FILEID
PDIV2 2 Main
PAGE2
PAGE3
PAGE4 3
PAGE5 4
PAGE6 5
PAGE7 6
PAGE8 7
PAGE9 8
PAGE10 9
PAGE11 10
PAGE12 11
PAGE13
PAGE14 13
PAGE15 14
PAGE16 15
PAGE17 16
PAGE18 17
PAGE19 18
PAGE20 19
PAGE21 20
PAGE22 21
PAGE23 22
PAGE24 23
PAGE25 24
PAGE26 25
PAGE27 26
PAGE28 27
PAGE29 28
STRUCT2 other
ODIV1
FILES1
FILES2


xml version 1.0 encoding UTF-8
REPORT xmlns http:www.fcla.edudlsmddaitss xmlns:xsi http:www.w3.org2001XMLSchema-instance xsi:schemaLocation http:www.fcla.edudlsmddaitssdaitssReport.xsd
INGEST IEID EHYQTFUG6_RM8A96 INGEST_TIME 2017-04-11T19:01:18Z PACKAGE UF00001180_00001
AGREEMENT_INFO ACCOUNT UF PROJECT UFDC
FILES


xml version 1.0
xml-stylesheet type textxsl href daitss_report_xhtml.xsl
REPORT xsi:schemaLocation 'http:www.fcla.edudlsmddaitss http:www.fcla.edudlsmddaitssdaitss2Report.xsd' xmlns:xsi 'http:www.w3.org2001XMLSchema-instance' xmlns 'http:www.fcla.edudlsmddaitss'
DISSEMINATION IEID 'E20080903_AAACDG' PACKAGE 'UF00001180_00001' INGEST_TIME '2008-09-04T08:54:01-04:00'
AGREEMENT_INFO ACCOUNT 'UF' PROJECT 'UFDC'
REQUEST_EVENTS TITLE Disseminate Event
REQUEST_EVENT NAME 'disseminate request placed' TIME '2017-03-09T12:32:01-05:00' NOTE 'request id: 310138; E20080903_AAACDG' AGENT 'UF73'
finished' '2017-03-09T12:36:58-05:00' '' 'SYSTEM'
FILES
FILE SIZE '40829' DFID 'info:fdaE20080903_AAACDGfileF20080904_AABUMZ' ORIGIN 'DEPOSITOR' PATH 'sip-files00001.jp2'
MESSAGE_DIGEST ALGORITHM 'MD5' 26bc33a9a2af4789876d0fa27744f91d
'SHA-1' bd0f0fda1a6552fb12d6442cff0f437206793873
EVENT '2017-03-09T12:33:25-05:00' OUTCOME 'success'
PROCEDURE describe
'37983' 'info:fdaE20080903_AAACDGfileF20080904_AABUNA' 'sip-files00001.jpg'
fd02181a24aae0058bc782828f77fcf1
1d82a78eedb16bf387bc03d1d119d7ee014b6749
'2017-03-09T12:33:54-05:00'
describe
'17099' 'info:fdaE20080903_AAACDGfileF20080904_AABUNB' 'sip-files00001.pdf'
d37c675547c4b9a88fe0c3b2437c6fc7
a3dcefa7016e01d9f36706a28096c4a76eb4b0f4
'2017-03-09T12:33:10-05:00'
describe
'35577' 'info:fdaE20080903_AAACDGfileF20080904_AABUNB-norm-0' 'ARCHIVE' 'aip-filesF20080904_AABUNB-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T12:34:07-05:00'
describe
'2017-03-09T12:33:12-05:00'
normalize
'12880' 'info:fdaE20080903_AAACDGfileF20080904_AABUNC' 'sip-files00001.pro'
eb8599221fb2111ca8b51932e1cd9673
628f8f6fb643ae55c8c5d1985d5498a43accbb31
'2017-03-09T12:33:52-05:00'
describe
'12521' 'info:fdaE20080903_AAACDGfileF20080904_AABUND' 'sip-files00001.QC.jpg'
312936e87118a6b46d70c4ba52b4831d
8ccbaacc7f0893398a0c3a2a6dead09ec842b4d8
describe
'934668' 'info:fdaE20080903_AAACDGfileF20080904_AABUNE' 'sip-files00001.tif'
b78db77041584846f6575c8584a5528e
ee84be1ac511767a4b19466b296acfc956e21bd0
'2017-03-09T12:32:42-05:00'
describe
'705' 'info:fdaE20080903_AAACDGfileF20080904_AABUNF' 'sip-files00001.txt'
d94d54c3d87ac787886d99be9a3b699b
e8af46cbcebc7ad1bcbf705dae1249b4367852a9
'2017-03-09T12:33:53-05:00'
describe
'4313' 'info:fdaE20080903_AAACDGfileF20080904_AABUNG' 'sip-files00001thm.jpg'
143e50553f3d0537767e33cb41076f56
a9f99ea87b5c8f56599f41e7c36c7e4220af1f88
'2017-03-09T12:33:50-05:00'
describe
'102612' 'info:fdaE20080903_AAACDGfileF20080904_AABUNH' 'sip-files00002.jp2'
3da3961a196bcf5a60c3e7360dc1797a
e7256288110b369fe6540bb0f25664bf15af9644
'2017-03-09T12:32:35-05:00'
describe
'96790' 'info:fdaE20080903_AAACDGfileF20080904_AABUNI' 'sip-files00002.jpg'
da1a2b4ff3f69c8df24a6ebb3c96efd7
fb9d788698cc2f52aa19873289226d612d7cf15e
'2017-03-09T12:33:31-05:00'
describe
'40761' 'info:fdaE20080903_AAACDGfileF20080904_AABUNJ' 'sip-files00002.pdf'
6e2a52f84df3bfb6653f1c207fdba46b
80e979770938111698d3c17ccc5f32a6ce151f81
'2017-03-09T12:33:13-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUNJ-norm-0' 'aip-filesF20080904_AABUNJ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T12:34:10-05:00'
describe
'2017-03-09T12:33:15-05:00'
normalize
'29443' 'info:fdaE20080903_AAACDGfileF20080904_AABUNK' 'sip-files00002.pro'
f683015214bdc349173c3140a7823051
a91ec53b6809649a898740413d0c5fd285161b2a
'2017-03-09T12:33:17-05:00'
describe
'31983' 'info:fdaE20080903_AAACDGfileF20080904_AABUNL' 'sip-files00002.QC.jpg'
10238e78694130b115019ba6d3b64ed1
fddd4c517a7c32faa59461b9f0821db9daa59491
describe
'960824' 'info:fdaE20080903_AAACDGfileF20080904_AABUNM' 'sip-files00002.tif'
b1d3e0fa5d20c618c6af2e6337c48a83
96f05e124e066944699fff9bc8bb6c9f787bd561
'2017-03-09T12:33:08-05:00'
describe
'1346' 'info:fdaE20080903_AAACDGfileF20080904_AABUNN' 'sip-files00002.txt'
addd9c63059d4d86a9c34b5396aceee7
3104ed25cbb35f263d4953eb30a5d7732b951d6b
'2017-03-09T12:33:07-05:00'
describe
'8825' 'info:fdaE20080903_AAACDGfileF20080904_AABUNO' 'sip-files00002thm.jpg'
492dca43a7500e9fb5642ef29540ad12
5275c33af83b42fca304f71f3488eb38cfdcc887
describe
'145108' 'info:fdaE20080903_AAACDGfileF20080904_AABUNP' 'sip-files00003.jp2'
aa3d743e3bb8d6e7522651e94ef07170
9d27c2146643e00be6792d0fbd80902bfe0ed268
describe
'156212' 'info:fdaE20080903_AAACDGfileF20080904_AABUNQ' 'sip-files00003.jpg'
8c64f017bdc1114f91bf96e4dfa0989b
d76dbbaa46fe433f0724bd0bc7f3ec30f7f1aada
'2017-03-09T12:33:49-05:00'
describe
'58847' 'info:fdaE20080903_AAACDGfileF20080904_AABUNR' 'sip-files00003.pdf'
2551504b6225e4edeaad934937c3788a
67a0ff284ecdebbc0ddbae2ee8b5cc41067d8f64
'2017-03-09T12:33:39-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUNR-norm-0' 'aip-filesF20080904_AABUNR-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T12:34:06-05:00'
describe
'2017-03-09T12:33:41-05:00'
normalize
'47724' 'info:fdaE20080903_AAACDGfileF20080904_AABUNS' 'sip-files00003.pro'
217e985a6cec06e69c19866416a127b6
b9c8e8ef080e38d34e4d73aab5a1553aefe9fc68
'2017-03-09T12:34:03-05:00'
describe
'52399' 'info:fdaE20080903_AAACDGfileF20080904_AABUNT' 'sip-files00003.QC.jpg'
9e6a0737db9c1445914fab902c95adfe
8ade34b6e690101380b06c851716d06fcd96c9b3
describe
'899532' 'info:fdaE20080903_AAACDGfileF20080904_AABUNU' 'sip-files00003.tif'
6e505b3f83f2cd64f1fee546fc1c1735
5f0358a21f430e310d55dcaf1110dba3acf037cf
'2017-03-09T12:32:36-05:00'
describe
'1817' 'info:fdaE20080903_AAACDGfileF20080904_AABUNV' 'sip-files00003.txt'
3fa83c240630d3bb62d29240a615d8df
ef2042a445e1bc1b196b6bd8946c68b1b607bb80
describe
'13513' 'info:fdaE20080903_AAACDGfileF20080904_AABUNW' 'sip-files00003thm.jpg'
7fdcdd9aa2352f8ea0c32a0e07cbed2e
40e6d9fd90b66ba37d320a3820a6a76d0792a413
describe
'146511' 'info:fdaE20080903_AAACDGfileF20080904_AABUNX' 'sip-files00004.jp2'
415357964170602996b6bae25b764a1a
7ade21d7b4f96081ab9f723ec1850fd8d8aa5131
'2017-03-09T12:32:45-05:00'
describe
'145281' 'info:fdaE20080903_AAACDGfileF20080904_AABUNY' 'sip-files00004.jpg'
4092b5a1dec7aacd97869be1e20e4678
715c60c17beaeb244d04d9ec9fe75f673ad2b3d9
'2017-03-09T12:32:37-05:00'
describe
'58858' 'info:fdaE20080903_AAACDGfileF20080904_AABUNZ' 'sip-files00004.pdf'
d387ee29e88fb96b0e77cea7313171ec
808b6e079aaaa1061e27d577e85ebcefd6e8ee18
'2017-03-09T12:32:48-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUNZ-norm-0' 'aip-filesF20080904_AABUNZ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:32:50-05:00'
normalize
'47453' 'info:fdaE20080903_AAACDGfileF20080904_AABUOA' 'sip-files00004.pro'
3c9c853b63734598f54ee32394a913bf
1abd04c8f9116eb054da3405f0787d6a839ee1db
'2017-03-09T12:32:55-05:00'
describe
'48883' 'info:fdaE20080903_AAACDGfileF20080904_AABUOB' 'sip-files00004.QC.jpg'
d8d6c975ea16e13cc6ae27b93f48d431
38a59a90e7313ca3cad8434d8fd2ed2aef492b60
describe
'954324' 'info:fdaE20080903_AAACDGfileF20080904_AABUOC' 'sip-files00004.tif'
32168198da951cd6d64ec52658a72d7a
a57432231be2002b6e7ea0759c911cf8418cf4b0
describe
'1796' 'info:fdaE20080903_AAACDGfileF20080904_AABUOD' 'sip-files00004.txt'
ce88ec4c31aeae6724e771835895846f
54416165720cc964b60d703938f28d3e2490e845
describe
'12787' 'info:fdaE20080903_AAACDGfileF20080904_AABUOE' 'sip-files00004thm.jpg'
ae7a10831fbe1678df9fbc5b5b35ce7e
1eb6bc10ff1731f82e4548153e256152474283eb
describe
'153849' 'info:fdaE20080903_AAACDGfileF20080904_AABUOF' 'sip-files00005.jp2'
a3fcae26979c96ed74dd345c8186b652
c88bc2ec8e907a5bff0864616f8b8b704fd69232
describe
'154631' 'info:fdaE20080903_AAACDGfileF20080904_AABUOG' 'sip-files00005.jpg'
c0a0146b559fc4cd37c5a1fb064b4936
ad449d2d05868abb3cce12b6f59c6ecb1d186813
describe
'63198' 'info:fdaE20080903_AAACDGfileF20080904_AABUOH' 'sip-files00005.pdf'
633534f7607d971126a24b7609a9aa4b
4709c9ad0046ac7d2357d5cabf90c8b0da7b2b12
'2017-03-09T12:33:28-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUOH-norm-0' 'aip-filesF20080904_AABUOH-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T12:34:08-05:00'
describe
'2017-03-09T12:33:30-05:00'
normalize
'49510' 'info:fdaE20080903_AAACDGfileF20080904_AABUOI' 'sip-files00005.pro'
8445b0c408c80dcedf4ae67df24ad274
c2438c779ef2faa4a86fa20c056cf4110612cd8d
'2017-03-09T12:33:48-05:00'
describe
'52958' 'info:fdaE20080903_AAACDGfileF20080904_AABUOJ' 'sip-files00005.QC.jpg'
23404bf2854163bdc3d97400e78e258b
89659d56585a3d80628bbcb34c9d71bb7589272c
describe
'927636' 'info:fdaE20080903_AAACDGfileF20080904_AABUOK' 'sip-files00005.tif'
8f9e7b9ce51a949f304d7e2af39dfaf7
05da0f797b7cf59a93543c92b53cd0e0ffeea2ab
'2017-03-09T12:33:45-05:00'
describe
'1861' 'info:fdaE20080903_AAACDGfileF20080904_AABUOL' 'sip-files00005.txt'
02b8f5b6d0159e68f8b419e857dedfa9
34db171b5d3cd5fe20eb9a1cc49f876068b4bf85
describe
'13251' 'info:fdaE20080903_AAACDGfileF20080904_AABUOM' 'sip-files00005thm.jpg'
4538459bd566724aa756ae892b646713
2192d36fef6790aff2405d9d037bcab7a2f56564
'2017-03-09T12:33:44-05:00'
describe
'80241' 'info:fdaE20080903_AAACDGfileF20080904_AABUON' 'sip-files00006.jp2'
e61a61f68487f32911b8c049c91f72ae
32c11623eb34b42cfcc8ac58ff3649c5a389c519
'2017-03-09T12:33:34-05:00'
describe
'78959' 'info:fdaE20080903_AAACDGfileF20080904_AABUOO' 'sip-files00006.jpg'
afeabe3925afcd46d20ac940dd9c5281
be08c71becf8bae3c18a40c076c0a284012d5bfc
'2017-03-09T12:33:20-05:00'
describe
'32946' 'info:fdaE20080903_AAACDGfileF20080904_AABUOP' 'sip-files00006.pdf'
e85816ac8e7220759a793dc18a245299
c4ba436236872989cadbfb1bf886213c2cdd0db6
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUOP-norm-0' 'aip-filesF20080904_AABUOP-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:32:44-05:00'
normalize
'24106' 'info:fdaE20080903_AAACDGfileF20080904_AABUOQ' 'sip-files00006.pro'
8dc8b00eeb398c51ac7039fb06508ac4
e62efe58e2a57fd621222e6c1ce009f7e8fd0402
describe
'26234' 'info:fdaE20080903_AAACDGfileF20080904_AABUOR' 'sip-files00006.QC.jpg'
698c76612ef27fe6f3594688bf3fa3ed
a42b1708fee75d9c5bd7f6ac21cb13a6674500e7
'2017-03-09T12:33:22-05:00'
describe
'959344' 'info:fdaE20080903_AAACDGfileF20080904_AABUOS' 'sip-files00006.tif'
e7c04bdaf48019fb8c3c1969fe427cc6
732c56cf913531a72cfc422fb218e87da4d664b8
describe
'903' 'info:fdaE20080903_AAACDGfileF20080904_AABUOT' 'sip-files00006.txt'
42a838d321a279adc03ddd6afcbc3c1b
8b2b315a9df9f29ab38006aea9ff789c72dcb66e
describe
'7020' 'info:fdaE20080903_AAACDGfileF20080904_AABUOU' 'sip-files00006thm.jpg'
f7ccab5aa808b8b8eef3f587960ef7dd
e7e68f397e4ecc31bd21b655160ebf3d3e2d4f53
describe
'82198' 'info:fdaE20080903_AAACDGfileF20080904_AABUOV' 'sip-files00007.jp2'
e3bf8de68bdf69c39380f6b57157d472
e696e0177b3df7bfac74a190097e697a96c6741a
describe
'76683' 'info:fdaE20080903_AAACDGfileF20080904_AABUOW' 'sip-files00007.jpg'
967e09e9348cb79dec905c31755051a0
809c6a7e228dbc148623e89383ac251eea0d3284
describe
'33449' 'info:fdaE20080903_AAACDGfileF20080904_AABUOX' 'sip-files00007.pdf'
50f838f12a68e001ade06fc76b4520fb
8ed43ce9111227b240ffe66c36a281c7e4be5c4b
'2017-03-09T12:32:59-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUOX-norm-0' 'aip-filesF20080904_AABUOX-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:33:01-05:00'
normalize
'1738' 'info:fdaE20080903_AAACDGfileF20080904_AABUOY' 'sip-files00007.pro'
881ca9b9510fb6b3a2a85df6126c3daf
c93e23f72fc97eb1f20d71ec4ddd322268f37758
describe
'25355' 'info:fdaE20080903_AAACDGfileF20080904_AABUOZ' 'sip-files00007.QC.jpg'
1b5c37eadb28336b7e3412f52270c918
2d74a65c4f5b7ab657f16916dbf661390206067e
'2017-03-09T12:32:54-05:00'
describe
'882364' 'info:fdaE20080903_AAACDGfileF20080904_AABUPA' 'sip-files00007.tif'
22bf1b64b2a5877b5a682dfe5f07786f
fbfb38db2bbd541c56f9ac171c9e1395e383133f
describe
'133' 'info:fdaE20080903_AAACDGfileF20080904_AABUPB' 'sip-files00007.txt'
c44a3e430a37a1f7f71c660fb5a37ac3
822a81a349e2b75190eac792f7b49663bfb57cec
'2017-03-09T12:33:47-05:00'
describe
'7437' 'info:fdaE20080903_AAACDGfileF20080904_AABUPC' 'sip-files00007thm.jpg'
2ed88cbe2ffefc74a692b29408564bec
586f8adbb3f06be72d3735ad2e3182c4ac0e1ab4
describe
'125150' 'info:fdaE20080903_AAACDGfileF20080904_AABUPD' 'sip-files00008.jp2'
51e52f466b1a14adcdca4c916e217b95
9e1fd1eaaf7f423738697f29b3b1967df30e2bfd
describe
'122872' 'info:fdaE20080903_AAACDGfileF20080904_AABUPE' 'sip-files00008.jpg'
7c69390932827a37f3f6c3b6a55818f7
9f7310bed4e142949b5f19c7b9bd71114fdbed39
describe
'51068' 'info:fdaE20080903_AAACDGfileF20080904_AABUPF' 'sip-files00008.pdf'
735946460026ceace10d04156a3137cc
6957a998e043fb7d749a28ba98fd62c37378d599
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUPF-norm-0' 'aip-filesF20080904_AABUPF-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'36179' 'info:fdaE20080903_AAACDGfileF20080904_AABUPG' 'sip-files00008.pro'
6a2b81a3ea943df6d9c9a27b01528d88
99a5b03b66974f6c53212248548880ec59c4c955
describe
'40077' 'info:fdaE20080903_AAACDGfileF20080904_AABUPH' 'sip-files00008.QC.jpg'
6f10a431f2f070e5f7ef881080955d96
491a601bb86f8e665ab92f65368faf964dbb7abd
describe
'956628' 'info:fdaE20080903_AAACDGfileF20080904_AABUPI' 'sip-files00008.tif'
2eaac0d2d8089f65d374efb41b4688ad
fc827be9a9fde4e220c4895b1ba63c351b20e002
describe
'1479' 'info:fdaE20080903_AAACDGfileF20080904_AABUPJ' 'sip-files00008.txt'
bbcb5cc849ac6266df21f8fa030d4ae9
ec6b280c3c766b185b32c90df5677c39387fa0e8
'2017-03-09T12:33:59-05:00'
describe
'10620' 'info:fdaE20080903_AAACDGfileF20080904_AABUPK' 'sip-files00008thm.jpg'
ff1875610f0e74cc378af79e2b5ab752
259aa97d03d67c1b07d0fd19b6f447ba40459a62
'2017-03-09T12:33:06-05:00'
describe
'132793' 'info:fdaE20080903_AAACDGfileF20080904_AABUPL' 'sip-files00009.jp2'
4ba765e2b2c10384f6832b479ec6f96c
1b1b2d25f9b10adfb7ba44826b77f2b588fb13b8
'2017-03-09T12:33:55-05:00'
describe
'110415' 'info:fdaE20080903_AAACDGfileF20080904_AABUPM' 'sip-files00009.jpg'
628e54f798c44dc912d6cdb4abe2a959
a87e0514b7d5d155e3d9d581ea408f4b33dc74dd
describe
'61056' 'info:fdaE20080903_AAACDGfileF20080904_AABUPN' 'sip-files00009.pdf'
8aa8dbb589575b54743bdb1f53304158
07b955c5b1d504cd0df83680d29298c7e725f341
'2017-03-09T12:33:32-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUPN-norm-0' 'aip-filesF20080904_AABUPN-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'2802' 'info:fdaE20080903_AAACDGfileF20080904_AABUPO' 'sip-files00009.pro'
e23abc437546d2dc2970cafcc1955e75
e5f775df27baef478358d628c41ded9c3b499408
describe
'35249' 'info:fdaE20080903_AAACDGfileF20080904_AABUPP' 'sip-files00009.QC.jpg'
9eb50191a5eadafdcba0cb16071ad265
6625844b047c8a9705370502e87c4c291bc7cc64
describe
'973492' 'info:fdaE20080903_AAACDGfileF20080904_AABUPQ' 'sip-files00009.tif'
2bb601702b4bda2843f98e6e2281f9fe
aebe081108325495ab5bfb1abd6b1a8fd6e88b1f
describe
'167' 'info:fdaE20080903_AAACDGfileF20080904_AABUPR' 'sip-files00009.txt'
a36e419ded71500af66dd895e2abaebc
49e0a2ae55208dc05ef0bb6b6295dddc84ae5c43
describe
'10249' 'info:fdaE20080903_AAACDGfileF20080904_AABUPS' 'sip-files00009thm.jpg'
7aa936908969e03285cfb46415e4b120
a59d3fe3e6628f91fc30ccc5babbc160366bba7d
describe
'136757' 'info:fdaE20080903_AAACDGfileF20080904_AABUPT' 'sip-files00010.jp2'
2185fae73080403fb9916fa208ab20d0
b2d60b2a622fb066c09dbc80f1b0232e3aed0272
describe
'132513' 'info:fdaE20080903_AAACDGfileF20080904_AABUPU' 'sip-files00010.jpg'
29f4a638a62be9a7ac6b4be4c2a7b7fa
b340fcf945d9f7771daa8ec467c1947138c289ce
describe
'55186' 'info:fdaE20080903_AAACDGfileF20080904_AABUPV' 'sip-files00010.pdf'
d067bfa6839673313dd11ded013ecf80
3d96ed78ae4c32b0fd961dda6dc00405922e55dc
'2017-03-09T12:32:52-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUPV-norm-0' 'aip-filesF20080904_AABUPV-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'43894' 'info:fdaE20080903_AAACDGfileF20080904_AABUPW' 'sip-files00010.pro'
6cd1917db31ac018ce577bd3082719fb
82cba04cda4d2ab17df58ff36c47bd0d20e87065
describe
'43664' 'info:fdaE20080903_AAACDGfileF20080904_AABUPX' 'sip-files00010.QC.jpg'
982cd44321110f9c16c28df46bc5ea9e
ca3b2aae6ef2acc3a86a9b0639ba9e7bea2d3364
describe
'990712' 'info:fdaE20080903_AAACDGfileF20080904_AABUPY' 'sip-files00010.tif'
df45376e39b5e3e05a634704ce3d24f4
2cf00984e3a94a68493f78a9083c90f36b8a2995
'2017-03-09T12:34:00-05:00'
describe
'1664' 'info:fdaE20080903_AAACDGfileF20080904_AABUPZ' 'sip-files00010.txt'
caa8d7fd4a48243c7174356551f04612
10c75da39c7d0eb214b6694d1dd65f660c80af7a
describe
'11142' 'info:fdaE20080903_AAACDGfileF20080904_AABUQA' 'sip-files00010thm.jpg'
68f91907f97267375c572680c8b96281
67a6e7a0e3a6a31464253535db7739500de16eac
describe
'121372' 'info:fdaE20080903_AAACDGfileF20080904_AABUQB' 'sip-files00011.jp2'
926a23342b269648c6d801d75ad57537
42d873fd9bcadc0d5c2df985232b1874b38c4e48
describe
'124327' 'info:fdaE20080903_AAACDGfileF20080904_AABUQC' 'sip-files00011.jpg'
ae3f510b5c6427aa8118007470c5844e
843f1f04a19e3aea74b6a8a2ddc2cc3db20d8989
describe
'49088' 'info:fdaE20080903_AAACDGfileF20080904_AABUQD' 'sip-files00011.pdf'
2045d5062dfa8322a61d6ddd87adc333
3573cb9ace84f427514bc77ba6b0887c20079417
'2017-03-09T12:33:02-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUQD-norm-0' 'aip-filesF20080904_AABUQD-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T12:34:09-05:00'
describe
'2017-03-09T12:33:04-05:00'
normalize
'39972' 'info:fdaE20080903_AAACDGfileF20080904_AABUQE' 'sip-files00011.pro'
b17b71ae197101fde153af04fe386691
8c0d667b440e07d97eb0543ae19c7800a6910187
describe
'42293' 'info:fdaE20080903_AAACDGfileF20080904_AABUQF' 'sip-files00011.QC.jpg'
d5299aaf899c6e6b903d1593432c09f3
591872fc005e397fc08f393aa6a4281daae8c021
'2017-03-09T12:32:46-05:00'
describe
'941064' 'info:fdaE20080903_AAACDGfileF20080904_AABUQG' 'sip-files00011.tif'
41e1d60c8fcab945ec9e95f44e965b79
14b5aa4fafa9187c94bf79cb685756c117078018
describe
'1536' 'info:fdaE20080903_AAACDGfileF20080904_AABUQH' 'sip-files00011.txt'
be274926f4a0baf07d28c64ec3e071c4
2fe059dca74ed5bba69126b954caf3efb26600e6
'2017-03-09T12:33:37-05:00'
describe
'11161' 'info:fdaE20080903_AAACDGfileF20080904_AABUQI' 'sip-files00011thm.jpg'
5c90c6cd162dc820496459386fb3a426
8cabd63a3c1b4378efb80f179fcc29551a92cccf
describe
'122720' 'info:fdaE20080903_AAACDGfileF20080904_AABUQJ' 'sip-files00012.jp2'
ba53348c4f8e388208ca5f21aaaad27d
624665fdb721ea4ef53f496dc01e7e126bc7c35b
describe
'99214' 'info:fdaE20080903_AAACDGfileF20080904_AABUQK' 'sip-files00012.jpg'
49f869f98afcd9edc06a46c3623effb4
0f2b1cfb8778974f9c810c8d9f93cf8c5ffeb575
describe
'61417' 'info:fdaE20080903_AAACDGfileF20080904_AABUQL' 'sip-files00012.pdf'
0416dbdd4ac81211c5ae63bc4f056494
7df0877273e9a4e83b01d794157ec6eee5a048a0
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUQL-norm-0' 'aip-filesF20080904_AABUQL-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:32:57-05:00'
normalize
'5737' 'info:fdaE20080903_AAACDGfileF20080904_AABUQM' 'sip-files00012.pro'
d0758965084a20c8c814331a471f52b0
4adf26e108afde4fea1d18c5277dcba44719923e
describe
'28748' 'info:fdaE20080903_AAACDGfileF20080904_AABUQN' 'sip-files00012.QC.jpg'
d778464645e0920be979419cee561089
60accb4a5776045c9cb754aa8bb10de2c07e40e9
describe
'957080' 'info:fdaE20080903_AAACDGfileF20080904_AABUQO' 'sip-files00012.tif'
17d194f7d97eb2e397329402635f831f
1078c12ff40ef07f705440c8cfad7253a68284b0
describe
'219' 'info:fdaE20080903_AAACDGfileF20080904_AABUQP' 'sip-files00012.txt'
21dcd3aaff7ed44c709e8df39d7837b9
5d46a63a16eddce0d21654dcb8fa6aa89a296757
describe
'7504' 'info:fdaE20080903_AAACDGfileF20080904_AABUQQ' 'sip-files00012thm.jpg'
3134c402d0b224b076fade940e9aa6c4
e56ed0f636bf98fef8f4b7b796b341db40c5fec0
describe
'40545' 'info:fdaE20080903_AAACDGfileF20080904_AABUQR' 'sip-files00013.jp2'
fcd78cbb291ac965a86b225198395acd
c5031c9b00a3016b28bb0aba7d19080af4546b03
describe
'21176' 'info:fdaE20080903_AAACDGfileF20080904_AABUQS' 'sip-files00013.jpg'
e711a03bfa9162e1f1e8221f7e74525a
6c075f752e6af12d4aed6c0e49a0f4d5db4a6c93
describe
'17296' 'info:fdaE20080903_AAACDGfileF20080904_AABUQT' 'sip-files00013.pdf'
10dac6f72415d6023feb1762e90bcc35
0e2f584f2bb6a77cb1b9dae64848e141481965ce
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUQT-norm-0' 'aip-filesF20080904_AABUQT-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:33:27-05:00'
normalize
'2192' 'info:fdaE20080903_AAACDGfileF20080904_AABUQU' 'sip-files00013.pro'
120db0c9cb86138d65c42b9c70c22b8d
12775a1c744f661721ff5d6e4a9b44db9c3f9000
describe
'7358' 'info:fdaE20080903_AAACDGfileF20080904_AABUQV' 'sip-files00013.QC.jpg'
8f4021c2e6f167b6e447032b80a1e73a
63c4e492560b40a237463b3de91a0e38aaa54cf7
describe
'921848' 'info:fdaE20080903_AAACDGfileF20080904_AABUQW' 'sip-files00013.tif'
d9649e764ba3a9181f3d41a68fe1ba17
cfa347fa35e51c9f975e16fec4a5adfd92812903
describe
'113' 'info:fdaE20080903_AAACDGfileF20080904_AABUQX' 'sip-files00013.txt'
01a25a64ba2f31e7ee5692a2401c2f73
254e38aa013845e2eb6766dddc1a61b015964929
describe
'2635' 'info:fdaE20080903_AAACDGfileF20080904_AABUQY' 'sip-files00013thm.jpg'
27df5e248d135a41de0a096b1e34f44e
c3b702d7b953426ecba7949268844719aaebdf2b
describe
'118331' 'info:fdaE20080903_AAACDGfileF20080904_AABUQZ' 'sip-files00014.jp2'
a57fcd62f2c6b9cbf9cdebdcd1fc90b3
5b9f36b958a1364a0a01001fbd0c335e102cbf11
describe
'114908' 'info:fdaE20080903_AAACDGfileF20080904_AABURA' 'sip-files00014.jpg'
c6ca1da06d3453feb3c27323b7f906cc
7f7bbab45c3d8d8325ca80e29a4ad12d2f68ef58
describe
'48028' 'info:fdaE20080903_AAACDGfileF20080904_AABURB' 'sip-files00014.pdf'
a77981bcf5af5466398c13293566e487
b302b08588fd9d1e62a6525541e73bf8697f38dd
describe
'info:fdaE20080903_AAACDGfileF20080904_AABURB-norm-0' 'aip-filesF20080904_AABURB-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'36647' 'info:fdaE20080903_AAACDGfileF20080904_AABURC' 'sip-files00014.pro'
d4941ab0f95d4c2b96bf25b26a83d858
764d902dd68c296cd47705a207dce671e3e9e6a7
describe
'38443' 'info:fdaE20080903_AAACDGfileF20080904_AABURD' 'sip-files00014.QC.jpg'
5e7bce2ac8ec4826955fdfba17f54d4e
33a7161c51c9624494c7067a6ab4cadc7a66b802
describe
'961192' 'info:fdaE20080903_AAACDGfileF20080904_AABURE' 'sip-files00014.tif'
922501d7e602337789cf3391a64d479d
e84c2e7428f092d8b2e19050af34864b45c07292
describe
'1434' 'info:fdaE20080903_AAACDGfileF20080904_AABURF' 'sip-files00014.txt'
c9890a9f025b758a1d684c7ee4750b91
af0190bec0a67e91aa7b2717773813e964d9179f
describe
'10193' 'info:fdaE20080903_AAACDGfileF20080904_AABURG' 'sip-files00014thm.jpg'
41b274b133ed3df678fb62b67b1111d4
8e13cd88f2167e15ddf05a789f89f0c4c974a235
describe
'94639' 'info:fdaE20080903_AAACDGfileF20080904_AABURH' 'sip-files00015.jp2'
f7aa859554fcfd8e7e79bd8d3d7199c4
a54c5a2ede4abd255a52a07bf482ffc2346d0b80
describe
'85385' 'info:fdaE20080903_AAACDGfileF20080904_AABURI' 'sip-files00015.jpg'
cd04d205c3cb709caf9543d01805b3c6
de8a5e73ae8ef0abbf7170e21e7bfa8e8e25ea13
describe
'45330' 'info:fdaE20080903_AAACDGfileF20080904_AABURJ' 'sip-files00015.pdf'
b2c164cf00c2298b1ef44406ef0e72a5
eaaeab90fad4d7115aad97dcd41c7d7dced02551
describe
'info:fdaE20080903_AAACDGfileF20080904_AABURJ-norm-0' 'aip-filesF20080904_AABURJ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'9079' 'info:fdaE20080903_AAACDGfileF20080904_AABURK' 'sip-files00015.pro'
1c695d4d677986a04eedd7591f98c2f2
d2031af7f59b35686a3ba10217d0e94a3eb4a716
describe
'27766' 'info:fdaE20080903_AAACDGfileF20080904_AABURL' 'sip-files00015.QC.jpg'
a4460050fade5621dec97f87cfc3c6d9
6d41cf528c524d76780a3eaf71d8c76e515808ba
describe
'889552' 'info:fdaE20080903_AAACDGfileF20080904_AABURM' 'sip-files00015.tif'
a4cdc671d24609accfdae2f60d7b3012
b1b4fbba850b8696c7fe124add2d0e38b292ecf3
describe
'343' 'info:fdaE20080903_AAACDGfileF20080904_AABURN' 'sip-files00015.txt'
d34bffb5d3452bdd905f2d0da3eba5e7
f864f26d4d88d48732c39397c56dce863facd20b
describe
'7837' 'info:fdaE20080903_AAACDGfileF20080904_AABURO' 'sip-files00015thm.jpg'
a20e5af5f49bd0049d140e93d3e5d700
054df01a30eaeca7cb8ebee2bc779e97b4998219
describe
'172872' 'info:fdaE20080903_AAACDGfileF20080904_AABURP' 'sip-files00016.jp2'
0a1fe856fabf0ef485e859081f775051
8cae8682a967dbf5564e70952ceec2e030f5b1db
describe
'130997' 'info:fdaE20080903_AAACDGfileF20080904_AABURQ' 'sip-files00016.jpg'
227b94c9c92eea1dcc012e2f2b65378c
cc81b19cd3f35d88d070437dde311e513811c133
'2017-03-09T12:33:36-05:00'
describe
'83079' 'info:fdaE20080903_AAACDGfileF20080904_AABURR' 'sip-files00016.pdf'
572fdf519836ce514002f7870d67ca62
d5526eb3be3d1a6f01c8fd138d2d0a1d1f60afda
describe
'info:fdaE20080903_AAACDGfileF20080904_AABURR-norm-0' 'aip-filesF20080904_AABURR-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:34:05-05:00'
normalize
'23223' 'info:fdaE20080903_AAACDGfileF20080904_AABURS' 'sip-files00016.pro'
c8202479330fdf9380c950eff84f9b00
444711b55f51cb6ea595cfa0c0fe0a513de9ed97
describe
'40160' 'info:fdaE20080903_AAACDGfileF20080904_AABURT' 'sip-files00016.QC.jpg'
459e2679e4b332d47cc82aae0e562456
61f22f3877e54ffcdd2a042817794c946845b8c5
describe
'961692' 'info:fdaE20080903_AAACDGfileF20080904_AABURU' 'sip-files00016.tif'
ffa6d4b1f0b93b48d86f64e6f2e72499
fbe97cb4f1bfd9ad571944e3ea194a40559e941e
describe
'906' 'info:fdaE20080903_AAACDGfileF20080904_AABURV' 'sip-files00016.txt'
5e28430db763688f2b8ad0c6782d79bd
6a02c70fce2cb658f70a24c5599d3e3e10a6f7fc
describe
Invalid character
WARNING CODE 'Daitss::Anomaly' Invalid character
'10471' 'info:fdaE20080903_AAACDGfileF20080904_AABURW' 'sip-files00016thm.jpg'
18de484fdb3644f420ee6dbc7f349306
512f1fb415e6b5068d8c157fbb34762c2552c621
describe
'123348' 'info:fdaE20080903_AAACDGfileF20080904_AABURX' 'sip-files00017.jp2'
c891c84cb907b02b152e72c89a151f07
6b398e25f219a7ab7d7fdfd4ca16b1ffee5c887f
describe
'119854' 'info:fdaE20080903_AAACDGfileF20080904_AABURY' 'sip-files00017.jpg'
2d1e5574bd57789dc90265ef7d56d30a
553073c0acad9e56c4327a31b52ab1b4ff827786
describe
'49893' 'info:fdaE20080903_AAACDGfileF20080904_AABURZ' 'sip-files00017.pdf'
2eb4164fa2b9bfbc88948ca4dcf1a853
61c7f899b3b4a006813535b5f67ddcac4b06f06f
'2017-03-09T12:33:23-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABURZ-norm-0' 'aip-filesF20080904_AABURZ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:33:24-05:00'
normalize
'39723' 'info:fdaE20080903_AAACDGfileF20080904_AABUSA' 'sip-files00017.pro'
a4f8d2837dac6618525c74b1de0ec58c
1bec44883e5c249a80c3086d6ef11604fa3f5562
describe
'39607' 'info:fdaE20080903_AAACDGfileF20080904_AABUSB' 'sip-files00017.QC.jpg'
b94a5c03de5896051238faa648a1ce99
9b5dab5ed6b886e3f984e387f56d6d095d1db4a9
describe
'968828' 'info:fdaE20080903_AAACDGfileF20080904_AABUSC' 'sip-files00017.tif'
f2040ec0b4fd0476e514def00c920583
cd18319ed16efa05ea540bcf34f6042063341540
describe
'1502' 'info:fdaE20080903_AAACDGfileF20080904_AABUSD' 'sip-files00017.txt'
34b6937211a2efd1859e205f7be4cd1e
92171aab7670df2d05234c1ec4c24ddee4751230
describe
'10228' 'info:fdaE20080903_AAACDGfileF20080904_AABUSE' 'sip-files00017thm.jpg'
ba8bd9091bc143f3c827773dbf8f14aa
2369c89358368a81cfbf875aca4bd3836bfd104e
'2017-03-09T12:32:40-05:00'
describe
'194706' 'info:fdaE20080903_AAACDGfileF20080904_AABUSF' 'sip-files00018.jp2'
6c32b2111c77268578cb15d225943169
a389bbef564a14ee3707476c10db297a0049d669
describe
'135565' 'info:fdaE20080903_AAACDGfileF20080904_AABUSG' 'sip-files00018.jpg'
c366c7ebbf045ffe5332c7d15339c9e7
059ecb3cbf41c403ac2f5542bead5df6fc2fb871
describe
'91632' 'info:fdaE20080903_AAACDGfileF20080904_AABUSH' 'sip-files00018.pdf'
d2af55642df7ee9b7be7b498fbe0342b
4491292603a9de0b0441835b3896a2d53c361c3e
'2017-03-09T12:33:42-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUSH-norm-0' 'aip-filesF20080904_AABUSH-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:33:43-05:00'
normalize
'27530' 'info:fdaE20080903_AAACDGfileF20080904_AABUSI' 'sip-files00018.pro'
ebdd7951a6de89b9b90b625adbed0bfe
70f2f4283f435dd4d62bcbd1036c85622b4cec9a
describe
'41301' 'info:fdaE20080903_AAACDGfileF20080904_AABUSJ' 'sip-files00018.QC.jpg'
75238405cf709352eee7b217202d6687
e1dca839db927d84f254c549b7d89403fea3bca2
describe
'966360' 'info:fdaE20080903_AAACDGfileF20080904_AABUSK' 'sip-files00018.tif'
6379f210257e876776b926c2cd904e02
da94e01c97f7988111c97ff0da190e89e075df96
describe
'1065' 'info:fdaE20080903_AAACDGfileF20080904_AABUSL' 'sip-files00018.txt'
8c78912f4ad250f8d3fbe6e4316e86a6
3bae01749307b5ed7fe445d710f2243781c537d2
'2017-03-09T12:32:39-05:00'
describe
Invalid character
Invalid character
'10387' 'info:fdaE20080903_AAACDGfileF20080904_AABUSM' 'sip-files00018thm.jpg'
35fef9bd9b24f9c1c11c49264a7ed27a
4358303a8a570f0fea2dde419257c2bf8f4b63b1
describe
'48662' 'info:fdaE20080903_AAACDGfileF20080904_AABUSN' 'sip-files00019.jp2'
d850816cd8c6d559171d0d79ed72fb51
d505d7a4a0cb2de1e81876feb85870a4fab75d15
describe
'24889' 'info:fdaE20080903_AAACDGfileF20080904_AABUSO' 'sip-files00019.jpg'
ad1e714f2de0b0588865209377a50ca2
cac2140c3867241e9054e881929c71e7fdeeddf6
describe
'20394' 'info:fdaE20080903_AAACDGfileF20080904_AABUSP' 'sip-files00019.pdf'
9a94750b6ddde939709325cf965f93cc
41f48f12504bd53aa895e1a321e9e266efe8e718
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUSP-norm-0' 'aip-filesF20080904_AABUSP-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'2613' 'info:fdaE20080903_AAACDGfileF20080904_AABUSQ' 'sip-files00019.pro'
98f2a1eaa9ff4661484a038afe293e28
6411e05aba73273139748f0e4199d73ef06b04ac
describe
'8621' 'info:fdaE20080903_AAACDGfileF20080904_AABUSR' 'sip-files00019.QC.jpg'
e1ebe7863f88a671227d85e463ed73f8
afb5b47fb923def4d89d61b6491f3cb2a2e71662
describe
'868332' 'info:fdaE20080903_AAACDGfileF20080904_AABUSS' 'sip-files00019.tif'
7743e6e3d2a3af24c63a9c5e42428424
7cece8ecd6eb26a6a12158fbf28972d94ddb0e59
describe
'148' 'info:fdaE20080903_AAACDGfileF20080904_AABUST' 'sip-files00019.txt'
f77834be6f40e92bebbf944494e29aaa
37e958c8173049ce01abf1fc43b1a559c584aab0
describe
'3096' 'info:fdaE20080903_AAACDGfileF20080904_AABUSU' 'sip-files00019thm.jpg'
ef4ad644ad856a0988be9093f47f7ea8
1d4c217ec134a20ce4e37db35729acfc2936718c
describe
'85121' 'info:fdaE20080903_AAACDGfileF20080904_AABUSV' 'sip-files00020.jp2'
ead0ab0ae49458ebe75f107aeae9cc73
13d7441f4ba8b8fa1c9e001ed431fa3bef1d0b45
describe
'87019' 'info:fdaE20080903_AAACDGfileF20080904_AABUSW' 'sip-files00020.jpg'
0ed0ac3d03866aad7a93f9959bfe8ca3
f203744c27154a558faea8a86b629b2c86444da7
describe
'34724' 'info:fdaE20080903_AAACDGfileF20080904_AABUSX' 'sip-files00020.pdf'
4bab577e8afb18ab3b3a3c0964e49f53
931b18505e78e597cd36b9e957c9be6b065df463
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUSX-norm-0' 'aip-filesF20080904_AABUSX-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'23192' 'info:fdaE20080903_AAACDGfileF20080904_AABUSY' 'sip-files00020.pro'
d0ec3e9e9c736ffa5b68d4598a0b97af
2b27fa96fbff2c6af011fbec8ef8f7122358b915
describe
'28653' 'info:fdaE20080903_AAACDGfileF20080904_AABUSZ' 'sip-files00020.QC.jpg'
2ad9f9c42504a4ba9af69f50a65118de
5a8ec87a234dd6c02ec364f889fceaeccb698d6c
describe
'914360' 'info:fdaE20080903_AAACDGfileF20080904_AABUTA' 'sip-files00020.tif'
4094fb975d91044636cee5f1b8c92039
b13d833e8884191b88810a0f54a1aa6a2c4d6c58
describe
'958' 'info:fdaE20080903_AAACDGfileF20080904_AABUTB' 'sip-files00020.txt'
fb30ef565f5627f136db6b1978bf624f
1817332ec630224955ce32cb6e05123264333e32
describe
'7725' 'info:fdaE20080903_AAACDGfileF20080904_AABUTC' 'sip-files00020thm.jpg'
72c0c277474ad1fbf16f9a75cdb4eccd
0b9d58ffa31a18004985206136887d86f3e912d2
describe
'136282' 'info:fdaE20080903_AAACDGfileF20080904_AABUTD' 'sip-files00021.jp2'
8e3ae9c8567aef8cdd3b7e90411d2dd8
5f205ee5d438122e63a3fb06cc48fc522a9d410c
describe
'100110' 'info:fdaE20080903_AAACDGfileF20080904_AABUTE' 'sip-files00021.jpg'
4fa9a976fd6530d83ed2bcd2683bd91c
ae94bc7e41afa93ff0461c5f3c5a69f26062cff5
describe
'64279' 'info:fdaE20080903_AAACDGfileF20080904_AABUTF' 'sip-files00021.pdf'
fc9aa07103fbac17704dcda3fca14334
bac443fe249466886b7fb9abfeb76ce2e4d31bbb
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUTF-norm-0' 'aip-filesF20080904_AABUTF-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'11046' 'info:fdaE20080903_AAACDGfileF20080904_AABUTG' 'sip-files00021.pro'
9ea27983ec0f045a40fd92ed0a5f2ce7
4c0714fe487166bf505bd9e4e0b07fc33f9e122f
describe
'30742' 'info:fdaE20080903_AAACDGfileF20080904_AABUTH' 'sip-files00021.QC.jpg'
dde475241c44a0ab3e7eccf0616b5676
bd0898ad09b6b23e41918dd645eff90f1b0b989a
describe
'1010704' 'info:fdaE20080903_AAACDGfileF20080904_AABUTI' 'sip-files00021.tif'
a27fa8cc5bfb6abf5b242ad511cee509
c2f59d2584e4dbb9d0114f0b40375368c11c394b
describe
'503' 'info:fdaE20080903_AAACDGfileF20080904_AABUTJ' 'sip-files00021.txt'
e246d0fd438b2ac0fa0926ae3fa35438
92f66684bfe4a70bab3e4201f92de7937edefaed
describe
Invalid character
Invalid character
'8685' 'info:fdaE20080903_AAACDGfileF20080904_AABUTK' 'sip-files00021thm.jpg'
54138492281d9074a72833bdb113cab6
62ebd36849b92213c34ed0a103766e5eaeddaa76
describe
'166922' 'info:fdaE20080903_AAACDGfileF20080904_AABUTL' 'sip-files00022.jp2'
4c4702ab0c53b44d5f3adafe2f42a497
f53d9e9b056b7ff7f499c2a2f98a5f96397a620e
describe
'139716' 'info:fdaE20080903_AAACDGfileF20080904_AABUTM' 'sip-files00022.jpg'
c25690adf824f7e2dd91fdcbf314e990
e3604793346b183f41327c4ba4dd42881f9b47fb
describe
'80847' 'info:fdaE20080903_AAACDGfileF20080904_AABUTN' 'sip-files00022.pdf'
e0b29274ef5935975374a74a7ce79ca7
2f7ef7bea20a9e777f38137d809e023507c07b87
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUTN-norm-0' 'aip-filesF20080904_AABUTN-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'24233' 'info:fdaE20080903_AAACDGfileF20080904_AABUTO' 'sip-files00022.pro'
cc53b8c415c15658bc5409903f94415a
d5f8b144a92a8684f3139138a59abd23a83c7b9a
describe
'43219' 'info:fdaE20080903_AAACDGfileF20080904_AABUTP' 'sip-files00022.QC.jpg'
6812af65a6ed0eb1b87aeb0aa971470b
58a79bcd778b9b9e150077ad4d8fb150b5802cb1
describe
'936788' 'info:fdaE20080903_AAACDGfileF20080904_AABUTQ' 'sip-files00022.tif'
85bcf72995e7a338bec3b786cda1fc00
eba274f9b20a3b1150db00935363411266421b87
describe
'924' 'info:fdaE20080903_AAACDGfileF20080904_AABUTR' 'sip-files00022.txt'
5d6e8b2662d30c0b2db932487b908eb1
0d7b4b014b679dfd400fa0c0e45a2822c9f8fcee
describe
Invalid character
Invalid character
'11225' 'info:fdaE20080903_AAACDGfileF20080904_AABUTS' 'sip-files00022thm.jpg'
619c20e1c76b0ab0efc5c63cd4af2368
3751bbb49a39b2f4785c1cb31f9ecb5b138c23aa
describe
'134561' 'info:fdaE20080903_AAACDGfileF20080904_AABUTT' 'sip-files00023.jp2'
6ccf1b5d9a17a8a52d756a177cdd7276
948c7bcb3c30609116a0c32f1a961a9a28a65982
describe
'111356' 'info:fdaE20080903_AAACDGfileF20080904_AABUTU' 'sip-files00023.jpg'
59a3e973a1123f3a8fb7766b7a54a2da
7220c773a913accbffd36f4f0814e6394769b085
describe
'61804' 'info:fdaE20080903_AAACDGfileF20080904_AABUTV' 'sip-files00023.pdf'
1fbd3262c10b9ce9d3579b6c53bb4950
3ffdb0d0e9bd201d39429d7f273897a4c53e447c
'2017-03-09T12:34:01-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUTV-norm-0' 'aip-filesF20080904_AABUTV-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:34:02-05:00'
normalize
'18185' 'info:fdaE20080903_AAACDGfileF20080904_AABUTW' 'sip-files00023.pro'
da98d5bc0d0f665e8d60df402ad7b9d2
a7e9a1ecb4d94ab1fd58fae482a2ee31b13e251c
describe
'34850' 'info:fdaE20080903_AAACDGfileF20080904_AABUTX' 'sip-files00023.QC.jpg'
1bb4076638b83b0f67ab8f6509f7ecf3
3d1a34b52027d8f3ef9e134293951372f282be99
describe
'969000' 'info:fdaE20080903_AAACDGfileF20080904_AABUTY' 'sip-files00023.tif'
0bef9a934e6ab6e15be3a7d71b99d74c
7ee9141966d032447cbb6a150a673ae5e6ce59c8
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUTZ' 'sip-files00023.txt'
d66bc10cae1a62313064e81ed112aa7a
de91af5e1514558b606025aad6e6fc03acaf0dd5
describe
'9995' 'info:fdaE20080903_AAACDGfileF20080904_AABUUA' 'sip-files00023thm.jpg'
cb567f96e321ba68017d8c23386a1bc9
288f427a462d9f3b14cf2bdb13313037b2c47af6
describe
'171968' 'info:fdaE20080903_AAACDGfileF20080904_AABUUB' 'sip-files00024.jp2'
0e415c2d6d65f7226520de08d9f74a3c
98b695af392df40ae5c1bc3de2799c3cdea55cd4
describe
'136597' 'info:fdaE20080903_AAACDGfileF20080904_AABUUC' 'sip-files00024.jpg'
3ec50d52f58a091f0e60b985558ad8b1
1f536e4ca2890fb2b8ea066b92ca0437a3cf6ce9
describe
'87771' 'info:fdaE20080903_AAACDGfileF20080904_AABUUD' 'sip-files00024.pdf'
141a9fd3be7deb5aea48b3fe03ccd4ea
ac41b7eea7d5eeca4408e2a9e6dbc8553a4f8fa6
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUUD-norm-0' 'aip-filesF20080904_AABUUD-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'23878' 'info:fdaE20080903_AAACDGfileF20080904_AABUUE' 'sip-files00024.pro'
99ac1be6d3e7be03a4c712a928dcf2bb
db15b3756a734e5e214287b049d247b411407963
describe
'42453' 'info:fdaE20080903_AAACDGfileF20080904_AABUUF' 'sip-files00024.QC.jpg'
0a5476316a87619e14bdd5cb95881659
7b253416fc970eaef0a80fd07926cfef0579dbae
describe
'952416' 'info:fdaE20080903_AAACDGfileF20080904_AABUUG' 'sip-files00024.tif'
7bd111a9c1e6c2cdd6e76a055a94ad50
07ecfd11f2ce4207c98fda8d1815e7607fcb106f
describe
'949' 'info:fdaE20080903_AAACDGfileF20080904_AABUUH' 'sip-files00024.txt'
ce4b9df4f2476dc1225018244f38e1f1
4ce46912087e5d1f88e1b33a7b567efd80bb62c4
describe
'11095' 'info:fdaE20080903_AAACDGfileF20080904_AABUUI' 'sip-files00024thm.jpg'
1c1b473be3ef00b5125e2bc7d15d70fd
e646b0f7ebffddbcec32731dc4457c82b7597717
describe
'66566' 'info:fdaE20080903_AAACDGfileF20080904_AABUUJ' 'sip-files00025.jp2'
630b24a22ee70a4bff0f56bbc35f3298
e474b49f110946f8a74fbadd1b04ee8098203473
describe
'28890' 'info:fdaE20080903_AAACDGfileF20080904_AABUUK' 'sip-files00025.jpg'
108a5934370122c001fdd2cd56e6e4f9
ed55e1b98617c271985f3231258c203b235fdfa3
describe
'28501' 'info:fdaE20080903_AAACDGfileF20080904_AABUUL' 'sip-files00025.pdf'
b719db849e68441744f0d64a771386bc
e0bd423d5a7be82b0d37070f5408b151ae75df03
'2017-03-09T12:33:18-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUUL-norm-0' 'aip-filesF20080904_AABUUL-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T12:33:19-05:00'
normalize
'2874' 'info:fdaE20080903_AAACDGfileF20080904_AABUUM' 'sip-files00025.pro'
ba49928cab5e8c4f1ff27202ecdca6ab
9ae5433999e0a09bebaa2c6565bc74a3a899f960
describe
'9144' 'info:fdaE20080903_AAACDGfileF20080904_AABUUN' 'sip-files00025.QC.jpg'
7ce4ce731d8dbf25244f7f2097783946
933fd35778ae0108b295e544221970b09dbc61af
describe
'924432' 'info:fdaE20080903_AAACDGfileF20080904_AABUUO' 'sip-files00025.tif'
5e72583ec84eadf91e11957723ed1882
0b81eab588878f584a9a9166ac5fac0fa3522507
describe
'128' 'info:fdaE20080903_AAACDGfileF20080904_AABUUP' 'sip-files00025.txt'
be90bedc5675c77a0abf82b8ab5625ac
bf9e42de080457a53939f3dd6c58ef6a295c9b7e
describe
'3077' 'info:fdaE20080903_AAACDGfileF20080904_AABUUQ' 'sip-files00025thm.jpg'
41291dd29c943abd2b80958659d3dab6
d1fd3887386b25405232028a15123f69bd3ea5d9
describe
'127382' 'info:fdaE20080903_AAACDGfileF20080904_AABUUR' 'sip-files00026.jp2'
5c1490dd5e82bb9de64b4ca2df6a7358
1be0770464fe97391e4af5eee05f560ddbe1c5bb
describe
'124456' 'info:fdaE20080903_AAACDGfileF20080904_AABUUS' 'sip-files00026.jpg'
8e3223a695e0e615b2791615d1166134
409e898fa29b913f3d30878d57ccb306bc3a54c8
describe
'51625' 'info:fdaE20080903_AAACDGfileF20080904_AABUUT' 'sip-files00026.pdf'
0bfdb6aa6716f82961faff6cae56162a
bd9a3953b79179553cadb37ed7db3dd84019e637
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUUT-norm-0' 'aip-filesF20080904_AABUUT-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'37133' 'info:fdaE20080903_AAACDGfileF20080904_AABUUU' 'sip-files00026.pro'
2b0562bc69a03fe8b3cc64f2a112f820
8d1ce804a9eb0b1dd2fc2f34ef98b5edf0938a3e
describe
'40759' 'info:fdaE20080903_AAACDGfileF20080904_AABUUV' 'sip-files00026.QC.jpg'
c58a4d9867ab05e1663a3d69fe9d52b2
a112dd07a6cf708b83bbe13b6f98220959c20368
describe
'936624' 'info:fdaE20080903_AAACDGfileF20080904_AABUUW' 'sip-files00026.tif'
1f57ac4788fd6e33fcd7a0e1a8be8c04
dafbea4b168c5d55316e4cea1e8ac984d904bc3e
describe
'1450' 'info:fdaE20080903_AAACDGfileF20080904_AABUUX' 'sip-files00026.txt'
ad6a39727d33050117192ff3694638a8
0eab9e8732d2902b563989e18b70f2cdf543cd78
describe
Invalid character
Invalid character
'10765' 'info:fdaE20080903_AAACDGfileF20080904_AABUUY' 'sip-files00026thm.jpg'
77ef5d5dca8a21c224c14acdfc3e8317
241ffa53f4ba7a64f434462afaf9fffbb129b2af
describe
'133101' 'info:fdaE20080903_AAACDGfileF20080904_AABUUZ' 'sip-files00027.jp2'
30f12d7de225910f4cb5effcf1827f45
b5536545322e5ea79616c759b80da4630c4313b0
describe
'121131' 'info:fdaE20080903_AAACDGfileF20080904_AABUVA' 'sip-files00027.jpg'
df1ad7fca4687dc300d5d605bf2e2a23
b86b05b25276e90fb1ae67a3453095437463cd6e
describe
'61680' 'info:fdaE20080903_AAACDGfileF20080904_AABUVB' 'sip-files00027.pdf'
ecac9b5cd1d318fc5a15acdf1a4b789e
fe9d4178300398202b64e317b81e51eb83710a5e
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUVB-norm-0' 'aip-filesF20080904_AABUVB-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'19084' 'info:fdaE20080903_AAACDGfileF20080904_AABUVC' 'sip-files00027.pro'
cabdfa9f4174481b0e789d6ea8152785
e85822834030687d04fbec83bbe7eaf3493fe682
describe
'39337' 'info:fdaE20080903_AAACDGfileF20080904_AABUVD' 'sip-files00027.QC.jpg'
5522dba893e052bd4136c6d667f15d91
9777315698352fa9c5b7ab74401f4f343c328329
describe
'897328' 'info:fdaE20080903_AAACDGfileF20080904_AABUVE' 'sip-files00027.tif'
25f9e9073b00baf62a65a3227d19206c
78b64dbf9ee836eca87f5b7b27b99488f1b29b4d
describe
'781' 'info:fdaE20080903_AAACDGfileF20080904_AABUVF' 'sip-files00027.txt'
d45d38047adc2e2586f23e6bd81cdb60
975bdb4fe6287e43a14ca58fd1849a190aa508b8
describe
'10269' 'info:fdaE20080903_AAACDGfileF20080904_AABUVG' 'sip-files00027thm.jpg'
c334a46a801ab2277752f24e5e51616b
62eb8ef729d668133960393637d541056ff5a725
describe
'220295' 'info:fdaE20080903_AAACDGfileF20080904_AABUVH' 'sip-files00028.jp2'
d1fecbaf9098eecf8ea121d091580519
4d270bd3082bb246888e7db1beeb7c6fb16554b4
describe
'155716' 'info:fdaE20080903_AAACDGfileF20080904_AABUVI' 'sip-files00028.jpg'
c58fd547c6ee19677b9b18ded303c7fa
290b878ae15f45f36e6f1733cf24a039378965e9
describe
'103065' 'info:fdaE20080903_AAACDGfileF20080904_AABUVJ' 'sip-files00028.pdf'
c2a552c88d5bee99b1c903b2a8c4c550
e0b91c3299f758dc5f5d24b7accc2ad48bb0343d
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUVJ-norm-0' 'aip-filesF20080904_AABUVJ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'29069' 'info:fdaE20080903_AAACDGfileF20080904_AABUVK' 'sip-files00028.pro'
36c902ad052c10f6269fbe0d75b487ec
a4b667a4342cfdb75c33268626dcaf8c877875b9
describe
'46983' 'info:fdaE20080903_AAACDGfileF20080904_AABUVL' 'sip-files00028.QC.jpg'
ae09221be5c9e54751b70edd85ba80b8
5b20e996df947e8177d099be92bcb65a463f20ee
describe
'953628' 'info:fdaE20080903_AAACDGfileF20080904_AABUVM' 'sip-files00028.tif'
2faa52e7ad1d49911450a80a09016fe3
fdaf3ad069b91cdd4bd05bad59171ea55c94ce56
describe
'1183' 'info:fdaE20080903_AAACDGfileF20080904_AABUVN' 'sip-files00028.txt'
d2ae58e6bc5892ac7cd5ba840a8f11aa
f5f8c9f49d2e01acb1a9ddf33006d58e275b1333
describe
'11719' 'info:fdaE20080903_AAACDGfileF20080904_AABUVO' 'sip-files00028thm.jpg'
19a87e7093bb2ea99a9b50564cebdd83
5aa019790df3084a58c0b888531c0c0cbd4baf83
describe
'83450' 'info:fdaE20080903_AAACDGfileF20080904_AABUVP' 'sip-files00029.jp2'
1380c9308024d161cba61a1e58a68a4b
70384a8b5c9cd7417cc64419e311eca19469a7ee
describe
'73426' 'info:fdaE20080903_AAACDGfileF20080904_AABUVQ' 'sip-files00029.jpg'
a76afd42913968d7a0e661cb66a9db30
b8ff557b9443021573b40649a60aec481472fee8
describe
'39529' 'info:fdaE20080903_AAACDGfileF20080904_AABUVR' 'sip-files00029.pdf'
ded3acf1785321f14832d18b0998d29d
3f6aeb7cb423e16ea1701e7749965fdcb55aa3fe
'2017-03-09T12:33:09-05:00'
describe
'info:fdaE20080903_AAACDGfileF20080904_AABUVR-norm-0' 'aip-filesF20080904_AABUVR-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'8597' 'info:fdaE20080903_AAACDGfileF20080904_AABUVS' 'sip-files00029.pro'
76c97e8b7faa179bd27e33f06d8f5418
7e4f251dea48f3d0dcc66c3b9f31e83112d218cb
describe
'24389' 'info:fdaE20080903_AAACDGfileF20080904_AABUVT' 'sip-files00029.QC.jpg'
76a408be0c9872f8b06367a4252efbe5
499ac18c7ed961461c096e71a5ea7dcf7b8a4756
describe
'949628' 'info:fdaE20080903_AAACDGfileF20080904_AABUVU' 'sip-files00029.tif'
07d22419a0da0bdfe8432a86c503007e
24ae26719b7e5783979e911e6c262d0ff16de7ec
describe
'337' 'info:fdaE20080903_AAACDGfileF20080904_AABUVV' 'sip-files00029.txt'
3aeec0f83a8e3dd8615ea96f93fafb10
a3cd9c2b32e797e171a59f3e7ff2ce6dd51fda63
describe
'6585' 'info:fdaE20080903_AAACDGfileF20080904_AABUVW' 'sip-files00029thm.jpg'
cd2c24c75fe7b3b6e18c7b675f3ad067
3e0b9f97bc62be071bf348a1dba8e9c964b5b456
describe
'153168' 'info:fdaE20080903_AAACDGfileF20080904_AABUVX' 'sip-filescopyright.jp2'
cd965abaafb5da42dc6c8def20d374f4
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describe
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PAGE 1

Leaflet No. 12 Page Introduction.................................. ....... ......1 Suwannee River State Park.........................7 Ichetucknee Springs State Park...................13 O'Leno State Park.......................................19 Manatee Springs State Park........................25 On the cover: Limestone outcrop at Suwannee River State Park Prepared by Bureau of Geology Division of Resource Management Florida Department of Natural Resources 1982

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A GEOLOGIC GUIDE TO SUWANNEE RIVER, ICHETUCKNEE SPRINGS, O'LENO, AND MANATEE SPRINGS STATE PARKS by Ronald Hoenstine and Sheila Weissinger INTRODUCTION Much of North Central Florida is sparsely populated and retains the nearly-untouched beauty of "Original Natural Florida," the Florida that greeted the early European explorers. Located in this area of scenic rivers and sparkling springs are several popular state parks, including Ichetucknee Springs, Manatee Springs, O'Leno and Suwannee River. GENERAL TOPOGRAPHY Much of the area's distinctive beauty is associated with small and large solution depressions, springs, and disappearing rivers; topographic features representative of a general landform designated as "karst" by geologists. These features develop in limestone regions having plentiful rainfall. Sinkholes are numerous in the area, and are conspicuous features in the parks. SINKS Sinks occur as a result of the dissolution of limestone by the downward percolation of rain water. Rain combines with carbon dioxide in the atmosphere to form carbonic acid. As this aci1

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dic rain percolates downward through the soils it comes into contact and reacts with the underlying limestone. The result is dissolution of the limestone and the formation of cavities. As the cavities grow with time, the weight of the overlying sediments may cause collapse and the subsequent formation of a sinkhole. This process of formation may become accelerated in the future if this pristine area of Florida is subjected to increased amounts of acid rain. Some of these sinkholes are filled with water, while others are "dry sinks." While both groups of sinkholes may have continuity with the underlying limestone, the dry sinks permit rain water to percolate completely into the underlying limestone. SPRINGS Also associated with this karst terrain are numerous springs. Florida has long been famous for its springs. In fact, there are more large springs in Florida than any other-state, accounting for 27 of the nation's 78 major springs. It has been calculated that the total output of water from all of Florida's 300 known springs is around 8 billion gallons a day. To more fully appreciate how and why springs form, one must understand the term "aquifer." Hydrologists define aquifers as natural zones below the ground surface that yield water in quantities that are important economically. In this part of Florida the aquifer, which is known as the Floridan Aquifer, is a thick layer of limestone. This limestone is divided into formal units called formations. These formations, which vary in age and lithology (physical characteristics), include the Suwannee Limestone and limestone of the Ocala Group. Rocks must have two essential properties to 2

PAGE 4

be considered an aquifer. They must have porosity and permeability. Porosity refers to the openings in the rocks which have the capacity to store water. Such openings include cavities, voids or intergranular spaces. The second property, permeability, is equally important as it refers to the rocks' ability to transmit water through interconnected pore spaces. Although highly variable, parts of the Floridan Aquifer may contain as much as 30 percent open space capable of storing large quantities of water. Furthermore, the aquifer's permeability permits the movement of vast quantities of water to the surface via springs and wells. A spring occurs when groundwater from the aquifer is discharged as natural seepage or freeflow through an opening at the ground surface. The volume of water discharged may be small and form a trickle, or large enough to form a river, such as the Ichetucknee River. The volume discharged frequently varies, as it is dependent not only on porosity and permeability but other factors such as seasonal rainfall that recharges the aquifer, and pumpage, which depletes it. AGE OF THE GEOLOGIC FEATURES An age (time of deposition) of about 30 million years before the present, during a period of time known as the Oligocene Epoch, can be assigned to the limestone and dolomite which crop out in the Suwannee River State Park. An age of about 40 million years before the present (Late Eocene Epoch) can be assigned to the limestone occurring at the surface in the vicinity of Manatee Springs, Ichetucknee and O'Leno state parks. How do geologists determine the age of these rocks? A casual glance at the limestone 3

PAGE 5

exposed in these parks reveals the presence of marine fossils such as clams and oysters, while a closer microscopic inspection reveals numerous microfossils. Microfossils are the remains of tiny plants and animals that lived long ago. These organisms include, among others, the silicabearing plants called diatoms, calcareous marine algae known as coccoliths, and calcareous one-celled animals known as foramini-fera. The presence of microfossils in rocks serves as an important tool for various scientific groups, such as the Florida Bureau of Geology, in providing data for the dating of Florida's sedimentary rocks. Essential to the study of microfossils is the accepted principle that various species of plants and animals lived and died during certain periods of Earth's history. Therefore, the identification of these species, together with a knowledge of their life span, permits one to date the sediments in which they are found. ANCIENT ENVIRONMENTS Microfossils' small size, wide geographic occurrence, and abundance in sediments of all ages and diverse environments are characteristics that make them invaluable for the purpose of identifying ancient depositional environments. Specifically, microfossils can be important indicators of the water depths, temperature, salinity, and water currents that existed at the time the sediments were formed. For this reason, the utilization of microfossils has been of special importance in the study of Florida's past and in identifying the depositional environments that existed in the area of the four parks 30 to 40 million years ago. By comparing these microfossils with living relatives, we know that the sediments present in these parks were formed in a relatively shallow 4

PAGE 6

marine environment. In other words, the limestone you see in the parks was once covered by a shallow sea. The period of time when the Florida peninsula was underwater represents most of the last 200 million years of geologic history. The importance of microfossils to the study of Florida's past can be further illustrated by comparing the past environment of Florida to that of much of the rest of North America during the Cretaceous, a period of time that ended approximately 65 million years ago. During this period, when dinosaurs roamed much of North America, these parks, and indeed most of Florida, were underwater. This explains the absence of dinosaur remains in Florida. We hope this geologic guide will serve to enhance your enjoyment and appreciation of the beautiful and distinctive state parks of the Suwannee River Basin. 5

PAGE 7

EortI rks STATE PARKm 1-V4) ficn x-Dry Sinks Earthwarks Old Ste Road Ferry Lnding Columbus Cemetery SUWANNEE RIVER STATE PARK 0 1000 90 Feet

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SUWANNEE RIVER STATE PARK INTRODUCTION The confluence of the Withlachoochee and Suwannee rivers offers a unique and historic setting for the Suwannee River State Park. Visitors to the park are impressed with the quiet natural beauty of the rivers and the surrounding wooded uplands. Situated in the physiographic zone known as the Coastal Lowlands, the park's elevation ranges from a low of 40 feet above MSL (mean sea level) near the river to a maximum of 70 feet MSL near the eastern boundary of the park. THE RIVERS Originating in the Okefenokee Swamp of southeast Georgia, the Suwannee River winds through north central Florida past the park, continuing its journey to the Gulf of Mexico, its final destination. Similarly, the Withlacoochee River originates in south Georgia and flows southward to merge with the Suwannee River at the park, where this confluence of the two rivers can be viewed from a rustic overlook (see map). The distinct differences in sediment loads of the rivers can be observed from this vantage point. The light brown waters of the Withlacoochee are laden with suspended silts and clays which give the river a muddy appearance. In contrast, the Suwannee River is relatively free of suspended sediment. Its dark, brownishblack color is a result of high tannic acid content. This tannic acid is produced by decayed 7.

PAGE 9

View of Suwannee River The Confluence of the Withlacoochee and Suwannee rivers.

PAGE 10

organic matter which washes into the river from forests and swamps that line the shore. As the rivers flow southward they wind, or meander, resulting in rock and soil material being eroded from the outside and downstream side of river bends, while material is deposited on the inside and upstream side. You can observe this effect as you hike along the river trail. LIMESTONE EXPOSURES The effects of river erosion are evident in the park. As you walk southward along the river towards the earthworks and the overlook or northward along the river side of the Suwannee River Trail, you can observe limestone and dolomite outcrops on the south side of the river. The river has eroded the overlying sediments to expose these aged and weathered rocks. These limestones, which are part of the Suwannee Limestone, were deposited during Oligocene time (30 million years before the present). Through time, much of the limestone has experienced substantial dolomitization. This process occurs when limestone, composed of the mineral calcite (a calcium carbonate), becomes a different mineral, dolomite, through the substitution of magnesium for calcium. As a result the rock, which in its original state was porous and permeable, may become dense and impermeable. In addition, fossils usually become distorted or completely obliterated through this process of dolomitization. A close examination will reveal fossil shells, molds and worm borings exhibiting all degrees of preservation. West of the overlook is a prominent 9

PAGE 11

exposure of dolomite and limestone which, depending on the river stage, can measure more than 15 feet in height. SUWANNEE RIVER TRAIL Walking along the Suwannee River Trail one can not only observe limestone outcrops but also see low banks parallel to the river on the eastern side of the trail (see map). These low ridges, called natural levees, are formed as a result of the river flooding. As the river overflows its banks, an abrupt decrease in both water velocity and turbulence occurs, resulting in the deposit of the coarser particles of the suspended sediments. In time, these coarse deposits form ridges, or levees, which generally parallel the river's edge. SANDHILLS TRAIL The Sandhills Trail leads from the hardwood hammock along the river to the open forest of pines. Approximately 500 feet down the trail one can see several dry sinks on the northeast side (see map). These geological features, which have a diameter of approximately 20 feet and a depth of 10 feet, are collapsed limestone cavities (see "sinks", page 2). The trail continues to the Old Columbus Cemetery. The town of Columbus has long since disappeared, but some of its history remains on the weathered tombstones. One can see the results of weathering (especially the corrosive action of rain) on both the metal and stone markers. The once clearly legible monuments are now smooth due to the effects of rain and abra10

PAGE 12

sion from wind-blown sediments over a relatively short period of time. Imagine the effects of weathering on Florida's landscape over a period of millions of years. Dry sink along Sand Hills Trail 11

PAGE 13

Picnic ;,g\ Entrqnc 238) Area Station ICHETUCKNEE SPRINGS Launchi Areao j / -Blue A P Hole Blue Hole STATE PARK Access Trail Trestle Point Nature Trol l 0 2000 feet

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..ICHETUCKNEE SPRINGS STATE PARK INTRODUCTION South of Suwannee River State Park, strad,dling the Suwannee-Columbia county line, .is Ichetucknee Springs State Park, one of the most beautiful and popular parks in Florida. For many people its refreshing springs represent a cool oasis during the hot summer months. Elevations range from 25 feet MSL near the river to a maximum of 60 feet MSL in the western part of the park. The surrounding area has many features typical of a karst area. These include wet and dry sinks and numerous springs. THE SPRINGS Within the 2,241 acres that make up the park and along the upper reaches of the Ichetucknee River are nine named and many unnamed springs. The most northern spring is Ichetucknee Spring which forms the headwaters of the river. Nearby is Blue Hole Spring, which can be reached by a trail and boardwalk from the main park. Ichetucknee Spring is 75 feet wide and 105 feet long, and has a maximum depth of 14 feet. The spring has an average water temperature of 73oF and discharges 30 million gallons of water a day (based on measurements taken in 1975 by the U.S. Geological Survey). The trail just north of Ichetucknee Springs leads to Blue Hole (Jug) Spring (see map). This secluded spring with its crystal clear, blue 13

PAGE 15

waters is a favorite swimming site in the park. The spring is 85 feet wide, 125 feet long, and has a maximum depth of 37 feet at its north central end near the vent. The boil, which is clearly visible near the center of the pool, has a measured flow of 60 million gallons a day. View of Ichetucknee Spring and spring run 14

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LIMESTONE The spring's waters issue directly from the limestone aquifer. The exposed limestone which forms part of the aquifer in this park is the Ocala Group limestone of Eocene age. These limestones, which are approximately 40 million years old, contrast with rocks cropping out in the Suwannee River State Park in that the exposed limestones there are the Suwannee Limestone of Oligocene age (approximately 30 million years before the present). Thus, as we have come southward, we have taken a 10 to 15 million year journey back in time. The missing, younger, Suwannee Limestone, which would ordinarily overlie the Ocala limestones, was either never deposited here or was completely eroded over time. P-Limestone outcrop along Blue Hole Access Trail 15

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These limestones offer further contrast to those in Suwannee River State Park in that little dolomitization can be observed here. Because these rocks are primarily limestone (calcium carbonate), the fossils show better preservation. However, the calcium carbonate content of these rocks causes them to be more susceptible to dissolution by acidic rain. Similiar to the limestone exposed at Suwannee River State Park, these limestones, though much older, also once formed the bottom of an ancient, shallow sea. TRESTLE POINT NATURE TRAIL A walk along the clearly marked Trestle Point Nature Trail leads the visitor through hardwoods and pines that line the river (see map). Limestone outcrops of the Ocala Group can be seen along this trail at the river's edge. Directly across from Trestle Point you can see a tunnel formed by dissolution of the limestone. Other dissolution features observed along the river bank include cavities and irregular voids, many of which resemble caves and columns. These surface structures are very similar to features occurring in the limestone subsurface. Farther down the trail you can see a large, circular depression approximately 60 feet to the left of the trail. This depression is a dry sink which formed through dissolution of the underlying limestone by rain water. Several additional sinks similar to this one can be observed within the park boundaries. 16

PAGE 18

Continuing along the trail you will come to an overlook. This overlook permits you to see the remnants of an old hard rock phosphate mine which was being actively mined in the early 1900's. Note the trees' position and orientation with respect to the sloping sides. The distortion in their growing position is due to a process known as "soil creep." This process occurs as a result of gravity causing the slow, downhill movement of poorly-consolidated sediments, such as sands, that are present here. This movement, though very slow, has noticeable effects over time. The closest active phosphate mining today occurs in Hamilton County at a site approximately 40 miles north of the park. Phosphate represents one of Florida's greatest mineral resources and production in Florida exceeds that of any other state. i , Soil bank erosional features at Trestle Point 17

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StaQuarry STATE PARK Rjver nK Sink

PAGE 20

O'LENO STATE PARK INTRODUCTION A short drive south from Ichetucknee Springs State Park brings you to O'Leno State Park, located on the peaceful Santa Fe River. This interesting, scenic park has a general topography much like that of Ichetucknee, with numerous wet and dry sinks and limestone exposures. Elevations within its boundaries vary from a low of about 40 feet MSL to a maximum of approximately 79 feet MSL at the park's northwestern border. THE RIVER The Santa Fe River is fed by many springs and tributaries, including the Ichetucknee River, which joins the Santa Fe after a brief 5-1/2 mile journey from its headwaters. In contrast to the crystal clear Ichetucknee River, the waters of the Santa Fe are stained dark by tannic acid. The river's surface reflects like a mirror the luxuriant vegetation along the shore. 19

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A suspension bridge, built in the 1930's by the Civilian Conservation Corps, spans the river at the main park (see map). Below it is a small rapid, created when local dolomitic limestones were placed there as part of the construction of a mill that once stood on this site. Many limestone outcrops occur along the river and park trails. The suspension bridge spanning the Santa Fe River. 20

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THE LIMESTONE TRAIL Located to the left just past the park's entrance is the Limestone Trail (see map). This forest trail, which can be traveled in a leisurely 20-minute walk, presents the opportunity to observe numerous limestone boulders and are approximately 40 million years old, about the same age as those found in Ichetucknee Springs State Park to the north. In addition, one can observe an abandoned limestone quarry at the trail's overlook located on the northeastern side of the trail. Note the prominent limestone outcrop clearly visible at the south end of the quarry. Large quantities of limestone were mined from this now-inactive quarry for use in the construction of fireplace chimneys. As you continue your walk, you will see a large sinkhole to your left on the western side of the trail. 21

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RIVER NATURE TRAIL From the main park and just across the suspension bridge, one comes to the River Nature Trail (see map). This picturesque trail leads through lowland hardwoods and sandy pine forests within the river's flood plain. Several features of geologic interest can be observed along the way. Approximately 1,500 feet down the trail is a long, narrow lake. The water in this lake, which has direct access to the aquifer, fluctuates in response to groundwater levels. View of fake located on north side of River Nature Trail (water level responds directly to fluctuations in underlying aquifer). 22

PAGE 24

The next geologic feature of interest is the River Sink, which is located at the eastern end of the trail. It is here, observable from several vantage points, that the Santa Fe River disappears and flows underground for more than 3 miles before it again becomes a surface stream. The waters of the river are literally "swallowed up" by vertical, 100 foot deep conduits. These conduits channel the water downward into the subsurface limestones where the water travels laterally for several miles through cavities before reappearing at the surface. Such a phenomenon, creating what is known as a natural bridge, is not unusual in these regions of springs and sinks. As you leave River Sink you can see on the southern side of the trail, a large, shallow depression. Clearly marked with a park sign, this depression is a dry sink. River Sink 23

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FEET ENTRANCE MANATEE GirlSPRINGs' SPRINGS MANATEE SPRINGS Ln Large wsne STATE PARK Dock L APnd Bridge 3 wet sinks

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.MANATEE SPRINGS STATE PARK INTRODUCTION Manatee Springs is situated in a lush, semitropical, hardwood hammock just 23 miles northeast of the Gulf of Mexico. In addition to providing many recreational activities, the park contains excellent examples of karst landforms. The park is located in the physiographic zone known as the Coastal Lowlands, with elevations ranging from a low of near mean sea level at the river to a high of 25 feet above MSL in the park's interior. The area is rich in history, for these springs were known and visited for centuries by the Indians and early Spanish explorers. Today, thousands of tourists come to enjoy the sparkling, clear waters and tranquil surroundings. In the winter its namesake, the endangered Florida manatee, sometimes visits the springs to enjoy its constant 72°F temperature. THE SPRINGS The spring head, which is located 1,200 feet from the Suwannee River, discharges 4.8 million gallons of water per hour. The water issues from rock which is part of the Ocala Group limestone, the same limestone formation that is found in O'Leno and Ichetucknee Springs state parks to the north. These rocks, which can be observed as outcrops around the pool's perimeter, are approximately 40 million years old. An excellent view of the spring run can be 25 ."

PAGE 27

enjoyed from a boardwalk that leads from the boat launching area to the Suwannee River. Much of what may be seen as you walk along this boardwalk is similar to what was reported by William Bartram, a naturalist, in his visit to the spring in 1774. On this visit, he observed alligators, gar, catfish, mullet, trout, bream, pike and "the monstrous amphabious maneta (manatee)". He also noted great quantities of shells and shell fragments in and around the spring. A large underwater cave system extends 2,000 feet from the main spring. Scuba diving in these caves is very popular, but dangerous, and safety is emphasized by park personnel. View of the boil and spring run 26 * M26

PAGE 28

NATURE (SINK) TRAIL The Nature Trail begins at a point approximately one mile from the entrance station, just east of the camping area. This clearly marked trail leaves the main road and winds through a dense hardwood hammock toward the southeast. Visible on both sides of the trail are depressions, or sinks, of varying sizes and stages of development. Of particular interest is a series of three wet sinks located near the trail's end. Two of the sinks are connected by a narrow landbridge. This connecting bridge is underlain by rocks which have not experienced dissolution and subsequent collapse. In the future, the adjoining sinks may enlarge, engulfing the bridge. Two much larger sinks can be observed in the nearby camping area (see map). These sinks, which are filled with water, are connected via a network of underground solution channels to the main springs. q ........ ...-... .. ..=.. Information markers throughout the parks provide visitors with trail guides and descriptions of special features. 27

PAGE 29

Two of the sinks are connected by a narrow landbridge. This connecting bridge is underlain by rocks which have not experienced dissolution and subsequent collapse. In the future, the adjoining sinks may enlarge, engulfing the bridge. One of several wet sinks located along the Sink Trail. 28