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Citation |
- Permanent Link:
- http://ufdc.ufl.edu/UF00094371/00001
Material Information
- Title:
- Geologic map of Manatee County, Florida ( FGS: Open file map series 50 )
- Creator:
- Campbell, K.
- Place of Publication:
- Tallahassee
- Publisher:
- Florida Geological Survey
- Publication Date:
- 1993
- Copyright Date:
- 1993
- Language:
- English
Subjects
- Subjects / Keywords:
- Erosion ( jstor )
Sand ( jstor ) Quartz ( jstor )
Record Information
- Source Institution:
- University of Florida
- Holding Location:
- University of Florida
- Rights Management:
- 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.
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Full Text |
FGS070193
OPEN FILE MAP SERIES No. 50
R16E --
R17
R 18E
R19E
R21 E
FLORIDA GEOLOGICAL SURVEY
DEPARTMENT OF NATURAL RESOURCES
R23E
R22E
THIS IS AN INTERIM GEOLOGIC MAP.
EDITING AND EDGE MATCHING HAVE
NOT BEEN COMPLETED. UPDATING
AND CORRECTING ARE CONTINUING.
C'
C-
S A2 3 4 L 6KI
SCALE
GEOLOGIC MAP OF
MANATEE COUNTY
FLORIDA
BY
KEN CAMPBELL RG. #192
1993
Qsu Shell beds, undifferentiated. Includes sediments previously
placed In units primarily differentiated by the included
fauna (e.g the Caloosahatchee, Ft.Thompson, and Nashua Z
Formations, Pinecrest Beds).
Qu Undifferentiated surficial sands, clayey sands, clays, 0
marls and peats >20 feet thick. No formations U -
recognized.
O
< 0
TERTIARY Thpr u
Tha-Arcadia Formation (undifferentiated) of the Hawthorn Group. G1 O
Consists predominantly of carbonates which are variably --
quartz and phosphate sandy and clayey. Sand and day beds 0
are often present. Dolostone is generally the dominant
carbonate component except in theTampa Member. T hp
U i ii ~ Oi i ,
WALTER SCHMIDT
STATE GEOLOGISTAND CHIEF
Th npb-Bone Valley Miember or the Peace River Formaltion, Hawthorn
Group. Consists of pebble or gravel sized
phosphate fragments and sand-sized phosphate grains in a
matrix of quartz sand and clay Percentages of the various
components are highly variable.
Thpr-Peace River Formation of the Hawthorn Group. Consists of
interbedded quartz sands, clays and carbonates, all ofwhich
are variably phosphatic
SARASOTA COUNTY
R16E --
-N-
4 I
27 4'
27 10'
R17E
R 18E
R19E
R20E
R23E
R21 E
R22E
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PAGE 1
CARTOGRAPHY BY JIM JONES & TED KIPER T 36 S T 37 S T 35 S 27 20' 27 30'T 34 S T 33 S 27 40'R 18 E R 21 E R 23 E 82 10' R 22 E 82 20' R 19 E R 20 E 82 30' H A R D E E C O U N T YSarasoto BayGULFOFMEXICO SCALE4 MILES 3 2 1 0.5 0 6 KILOMETERS 5 4 3 2 1 0 N 82 40' R 16 E R 17 E R 15 E 27 20' T 37 S T 36 S 27 30'T 35 S T 34 S T 33 S27 40' R 15 E R 16 E R 17 E R 18 E R 19 E R 20 E R 21 E R 22 E R 23 E 82 40' 82 30' 82 20' 82 10' D E S O T O C O U N T YH I L L S B O R O U G H C O U N T Y S A R A S O T A C O U N T Y S A R A S O T A C O U N T YS A R A S O T A C O U N T YTampaBayManateeRiverTerra Cela BayPalma Sola BayManateeLakeBRADENTONPalmetto 780l780l780l70l70l70l70l70l70lMyakka City l64l64l64l64l64l64 64l62l62l62l37l39l43l43l43l43l55l45l45l45l45l55l55l55l55lp75p75p75p75p75 75p 684l789l684l FLORIDAMANATEE COUNTYGEOLOGIC MAP OFWALTER SCHMIDT STATE GEOLOGIST AND CHIEF GSKEN CAMPBELL P.G. #192QhTHIS IS AN INTERIM GEOLOGIC MAP. EDITING AND EDGE MATCHING HAVE NOT BEEN COMPLETED. UPDATING AND CORRECTING ARE CONTINUING. E FLORIDA FGS070193 OPEN FILE MAP SERIES No. 50 Qu Qr Qsu Qsu T.1907 BY 1993 G EOLO I CAL SURVEYQh Tha Qh Qsu Tha Qsu Qsu Tha Qu Thpr Tha Thpr Qu interbedded quartz sands, clays and carbonates, all of which Thpr-Peace River Formation of the Hawthorn Group. Consists of matrix of quartz sand and clay. Percentages of the various phosphate fragments and sand-sized phosphate grains in a Group. Consists of pebbleor gravel-sized Thpb-Bone Valley Member of the Peace River Formation, Hawthorn carbonate component except in the Tampa Member. are often present. Dolostone is generally the dominant quartz and phosphate sandy and clayey. Sand and clay beds Consists predominantly of carbonates which are variably ThaArcadia Formation (undierentiated) of the Hawthorn Group. marls and peats >20 feet thick. No formations QuUndierentiated surcial sands, clayey sands, clays, fauna ( e.g. the Caloosahatchee, Ft. Thompson, and Nashua placed in units primarily dierentiated by the included QsuShell beds, undierentiated. Includes sediments previously peats. No formations recognized. Used in peninsular area QrHolocene uvial and lacustrine sands, clays, marls and deposits. Mostly beach and dune sands along present amounts of organic matter and clay associated with lagoonal Qh/QphHolocene sediments consisting of quartz sand with minorEXPLANATION are variably phosphatic. components are highly variable. recognized. Formations, Pinecrest Beds). coastline. No formations recognized. TERTIARY QUATERNARY only. Thpr Tha Qsu Qr Qu Qu Qu Thpr Qsu Qu FLORIDA GEOLOGICAL SURVEY DEPARTMENT OF NATURAL RESOURCES Qu Thpr Qu Thpr Qu Qu Thpb
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