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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