FLORIDA DEPARTMENT OF NATURAL RESOURCES

MAP SERIES NO. 79 BUREAU OF GEOLOGY


ENVIRONMENTAL GEOLOGY SERIES


GAINESVILLE SHEET





FLORIDA DEPARTMENT OF NATURAL RESOURCES
"SR.AR. u,.t. 6M T
BUREAU OF GEOLOGY




19718

INTRODUCTION
De_-opment of guidelines -or w-se management of Florida' natural


be based upon adequate geologic data for sudc lields as waste disposal,






eat re o f Teure Taage mnow las n the m anagement irghay e ighrmtl geologT c



2l0d T les lmaopng pndsbot 70 mieads wd re.l hetre y Lnvo n centra m penin
ao r eprode tsied e asiv1del a nud o1t the 1-1rea1 M and 1 o11 un-1



po m -s U n a I abo e19no arle 9 is d uCts tgla ns the I ls t
on.9rve R. dge, III rpo -hillsd B intendged wig l asonse G a a bao












op oflort h nurnu o 2 G Nolog rahy r hed a ouatoe spo w deahS
9oloa 9 1 1ur91e and l uhs e 9pul o 191 1o11 Stat eson e nvic g l
In dI 9 11s mapda Badfor -o dt wh 33 ur an, bnd9-
s 1o 1yi1 Te1nse, to he sialy trined st th e tesnaee l 4 U n Ion.
34.2 ,, Pro, 3 711 1. 1 1- 1 -.l, .1 11%, 1 -1 d 091a,1



-tk196o f anre s19 ag w as the Oc ,nli just o f t uIhe -. zIons t1 9 th11e





it tle d -n g l -1ogs t c 70ypon s _apind winser d a er6 incal c nto pophulan

9nra1 1r0o 1cu 70 o and o other im poesato proviadte w t 9h 1 wi 1r e a
In U .ds I l I ad ot allIubhsthed o and npubhs da I t. Iles








Inut re abld F reat ora t o-Bgy plus pueddhhdnd freps U S
1o81n Col Su1 rny nd19 a the hu C untr Sg9a9 ns1 e I s I
ACKNOWLEDGEMENT

LowsnsesTe ra nrd ln n 18 9s9 t r1 0nd C rld ik 9 t.1e U 1er ti,


REGIONAL SETTING







a T he rei n oth e aial ovr f i -sdy dpIo a d iby a su --N,
ft9e -o -Ter 11 kown a1The o]I pal1 9,phlt o1, 0. Iigh TIn s -uc ture1 1






yas dt-e d LI oc ated b one t19 at 5ins "t -1les1 Le e o aty c Tily
1 s,230 1s l and. 1 a bo-9 E 70 kie 1 d1 e, -0 eope d P eo l p eAi1 nsul9 r












unopalty Eocene a nd nheof, ramnette onwSepColutember 5wi6, 19a5t0rS e
1a -19s10ed 19t901y 9 po0 t -1ap I Mi-ensoe yn .u.Ger
sed a- Ili nn rIng the dIne -nd I llgl ond areas




Tuhe Io 1a119 p1 y d1sins11 th- m11 are p c d
sunnL Ton h L e th uo I d 1- 5e urph faures t.










..9111ta11 0,9 0the a1ea1an a 01 9)1111 9, 111
B 9,oks 9 -tidg,, FarIfd OI ll, Bel[ Ridge, HbiI Spitg Gap, D-6







G a9p S. e- and 199 h Hill, Mar Hdl, u- P t R g, a nt t I

91 N19 9 Highlad 1T Ca-stal17 sanos 1 0osi e1wl9uch f t9res1
t Ith e 119 19Cle 1, --- O1and 19P 19 19 -, 9 IIy 1-h and, th p -1

L7 b II9sIa -1 III 011199 11a 19 9pr119 III
_est by I If Mexio ..d U. -s by t h. If

910, o1 lb,,,- 301 No111t 291 Norh Th c I -.
II9 9- -,0 II LIy DL9Ie, G-19his,, A h O011-e -ount1 oy
p919ly show9n Taylo, L9 ayette. S 11991 Co 0b1, I Bradord,II

1are the9Su10ne, S 9t 1,,1. 0 01119, andi W0thlaoche 1


Most1f the119d, however, -1-1tain 1ewe residen ts i 1ta r1, e -1-e1 u
11,1 pop utIII n i, con ntr9d 9111 d III me1or le d 1910 01nsu
by ,c..nty I Aqlh,1 104,764 wth111, 61 1 ,ra, Mario 69,030 wt1,


19 wh119 _ra, Bradford 14,21 1 1 13 1 "1, 11 U -
9,1190-911 11 1 -1 1ol 1inelthe 196,dn--s -t1hhe19 i ensus




Ga9nes9 9 he]' gest 1 dfase11 t w M-11 y in th11I ar Its



































I...t


GEOLOGIC DISCUSSION

reslted Io ..i dep t ng ,ie E.- epoh (deposted fro

58 to 36 mllon years ago) and tIe Ogocene epoch (depo I ted from 36 lo

nds and clays (1111deposited 1from 25 mon years ago9 to pre111) of variable
9h10n w, h ...... .. e1,11 n1 g 9g1pod If on bly thicker
01 9 Iu Mos II th e Ipose iIt eng I the Iate Eo-ene O0a1 a
Group, although, I te 11. iIlnlty of Gulf Hammock hr e exposu1,es of1
thIe iate Middle Eoene Avon Pak Limestone Tie Avon Park Limestone
9is Ih old cppmb Ifr ion I F1lor id. T Ih Tetiay li m 1wn
p in ti "'p aa b elon" I. th e L.mI ston1 If Ohgole



n. Ie L Couty Is -ns-dy

and mmas They an als be very finely rystalIne and occasionally
C Ihmnatd (le.t inusg siltton ith be ant reaso e t the b IIIdolomite





ha-nd Tie coues repng ated .. tis ia, t latd fl II Avn




Park L ieste I., Pl neromes ts Ga orale folohge d poslote moe tern oA-on

21ark Lmesne1 ed111 by erIo 0951) 1,s "te9 0 asal bRr eys.do









W eilterst c ld he desrU I ep Is ae tran d etreeno e s awd-ppar ntl
Io.loa-d --js Iand Io eo t h-, maknin g It h e y odifyth recog nh e I s
Cn s1owtern9 conunu s l-ie III 111 so lo ca bh e des9d
eds in so u theLn Lestounty arough o at the p Ao area a L mestone












n Thu e ht n t h is posed `- partst sads111 clye 011111 I Df y sD .
ada ylor coi nltti .eing e qate d l h l tones hd t holog eans that le ,n y











Iitn I ocat hetpo1a1 -b ho111 t., 9en11111 ely wll d ar111 y Ie
a 1one Io 11, -olomite ,,d I wilhibi dfff ng deers f 11111h9














Tora In Te 1 cuyth hmstonperio ee, Tossgy P11 aocene a1ge a1 -


















T1g he1 1' f 1ne1 f to 90 m u and an s1ts rph1, units v l01mos9 the en0,9e
ptere ands ereonymad p werey bey iandantiehd aun I.
-Iwse D1 1 1 Co ..ty 991Id Ih S, h 9t-111,1 Ri911 It a I

This, en. 11 in9ormally t 111ed t e e o 11 mbe and o, t-




















th e Inh e loda exenin gs e d int o Tyo un11 y thre dimstinct lom1te.1


ghlwand nara y f iddy -e-11-st d Johns a R hve Ie-to 11 .-e lof 0
91e W 1h11 1191 1r 1, ey 1`1 -11o11119e 9ar1 111t


S19,1, nh a -d y others be1ng1,g 1 Uh C, ya,,l Ri119 T1t, Cryst
R10 9 I -mt- -ps o-t tem e 0-y o1 1te11 P-hah era
Laye,111, DI and Gllct9cou es t 0 I. theste AG-a and 19t91



Cr R n Wlh.i-1n1 I-19-1w 1 teisoelth1 logy11 y1

L TI- it-l -1 n u 1- I ol bia a-d Suwann,0 -,n1-1 and i1

9lt1od11 Th1 h11 st s 1111 1911- o 1 111h -1a -r y
hn It- io et191911) y ti Ii h bn sh d


9,1id h11]9and 191 1, ith -r, A Io are mmonly 1 1.ae -,111
s1ed ients o1 Mio -n 19,g o 9pe1119ly, a9M 9 IIIII 9 1hd 11I
H11.1wth I .r- ,11 I, -pe.d dn 11191 p I. 1 1119h11, q91111 nt 1 n1
I. p0 rts If -Ion CI ty Ti1 e 1 4-ho I, I1 I -ery 1 t1 er, 091 o11g1 1
119 11909 19 9- t 9011, dd Itd~, lyy nd, 1 1ndy 91 ys,
-Imts d ---n, h e d wIth 1phosphate1 gras



i, apparently a de111 y lut.on1 d -,11ty I 1 .1 -1,1g L- T1 0


T" e rn porin "of ieI p I "' thpysiogaphi p -
known as tie Gulf Coasal Lowlands Te lowlands begin at 1 e pre111 nt1
astlhne and e-tend t d to eastern GlchlSt, central Levy- and enral
Suwannee counties, _undedr b thett di,, e. t etit If i th
Low ,nds the1 e ar ,1 ral iver valley y lowlands and I-hre mar, e terra e
Theil terra s and asse11 1ed shorelines, beg, g wit the youngest, are
tie Sidver Blut. Pamhco, and Wicomico.
T1he S1 Bluff sho111 e s 11 ns-Idered to at aIn ,elvalon of 1 0,

-.-1c1ed with 911111 119 9 Th. m.-sh11 .11, etendig bit. 1 I1

I0 -1m d primay If Pl 1es n t rnt I I n In I --die9 ndrl i
by stones nd dolomites t a sallow depth In Diie, County, the Sde
ltn e a s ma d a n as ctr III e I in mle and S, als u 0i. r- -d by
masta] marshes The Saiver Bluff terrain is Try arrow n the portion to

Tbc P(15 1 hid h pr bly an taine 0a -t and t25 1ee,
e a disllntCt mark on Taylor County in the near arraneme t a Flats
. 15I 1.o 50 R1 t i1 11 dunes 11 that parallel e a st Tr e toe of h1 s strand
.m.e is marked bya e10-1 o nT Ioeto nemditi tath erc, S11-cdr Bi

In D e 1 Coun ly the9 Pamho e dipmen ts less well de1 e 1 d, bu tPI, licrra
-a P, 0 id9r9d tP e 19t bitween-111 1t -oo and 2519 eo,.011

The Northern ty d 111 91 d hio e ot y Ithai pe er alles th 9 n e
1ie it Die- Conty Itho mgh 11 1n be0 t 1 as e wII, nIo-therI P-Lh



1-l e9, ul does 1 wit. u. w e ll cors Su1ingL o n to -1 the g d aern 1






athe Alanune Ls a nd C rsins al ovey s the orrac e.san rean el

aneat4 aounte6 th and e o f sande an lmedan se etusom res, odu alg letone
ti There Venit pro 5bly le create p -e-tw n Ihes nrhe Levy,




doutly d, nlt c nt thle lhr iston d theology II IDsItn CPnlt
by ver v ley o shre l R ge and tIe n le nRd sern h I 1ont1
111 t1st 9 9not o9 the0 9on1 91111f m a nd 9 o cup ying 9 ntal
Leym9 on1 s9 l aswm py9e wetrekon s the W aec0c91 91- I I. 9I 1l9r






-on ler Flats and embankmd eLam go Pamo nts I tle di-es f
(14 911e 1 the-e Ti s h) s well ey m pfed b suntklae [99 e T I,0, aI l -l
d y m norlh to. Gtdrtt Co9 un..I 1cosing tIIe -nd 11th1 lo I a 1 endn
9I9 01 i1ty ol9 c 1w 1, 11 S-1 1 nd 9 a t i R i- T the i lhlgy .t,
Wlalall Al 1I'ill 1 9 "I i 9- I L l o ny a res Lon o nd I0 1- 1- t1 .. sy -d,
111 9o91 beig 19,-ldby T1n19 th.n..1Levy0n1I1l ... ...9l
"elsI Wh \ 91110 I. 9s 1u9e9 Le1t on. Verno 95 a1 nd Wh i
911979y lntcd ,1,l110,l)1i un1at h ,ty 1 uv 1lllowV e 1951 prml9o9n
0&d O .les 9 11967) --1019d III 9101090 01111were 91spos 1


919t9i) thr 9 is 119dthe I 1 wneln W -e1-on 1`lt 111-1 ediyll, 1
Clnefland hu I 1ii 111t9e ha oslbee 9R0de i 11no 111iT lhng sum po
y 1, the relate 1111ns du1ng Wd 9 c 1 11 th- 1. l-t1 o 1,e 1
9191m I II )1d, 9 IJd id Lon1 h 19 nd -1- .) ]].Jl.) ,Ny




and .u....[la e ou me, )lncfsnT 91eo le ..1 1'am t repo a e d b,,


B11er1en 1h 1 9u sclla nd L ol P 9l1mt n ll1d .(te lana d I lt,
test Jbded mean to teoel bn the wmaothey re Rweren ted by the s-nd




1111101 190 91hl10 .1199 111 1 111111 -.
111191y 1r1- Iid h010 1 -1 1 119 9,1) d as 11999119 I0
b0 9199I I, h 9e rok- )111 )99 -II drn, -- 001 0I. 0



T b1 0 bent1 h ln se end n111 1 1 the northen e I fre t

-1 1 -o1, 119 e 1 r 1.1 1 dge9 n eastwl d 119 1r1 s1nted t) 1
h 191d SaOnlli ) 9T 1 0 0t1e 91ns -ldos In 9ola I
inhea urel [ I n d regI zer th e en lan e Vhtoloey1 nnhgh Sp ,n,





(m9p, Dullo G 11p,1 o s1 ed I ie ild 9 ls S--dem Uplani -,
11ll B M -a il l,, n d g Iot on ldil It.- 1,ll1 10 -1 I'9








The1 b okv ,l1ing9ec cs t 11n, eatu 9 re1 19 o9 9 0 m s g
rs d jdcd to tI c In d Ihd pthlo w er a l toune T he,
drt, er ro n, w ch n t hr o g eeys p are a. i s s e .in lo me long


a ry nta i needhr0t 1Cont Thew t. ro11i t -,1 otthe k tl

on Lht od pm and] U edbth eW ts Ind mol th -th taprso w
1nds, 0tl9 11,90 b, 1arel s1ul. It ns R.-111-1 1 9 11910s I.1lit







9,olut 111-9l - the t11119911 11 glands 9191 w the0,1 0 mr 1h9,n



to 0themhh prs T- 11-91 m1,11, b he Santa ..o through th OLto
911 9n 0I9 n 09
90l 1 9ll, 11t19 0 1,91 119919119' 119[1 h lah 11 Hil9 ,,Ier i,,d

t19 911g1, 11tile 1 r 1111i 1 11i1 111 I99 91Dunelo 1 I 11G -
T1. 1 .1 1a'h.9111, 91-1d I t9119 f0t.a1es bro 0011em 10111,1





Marten 99 9o1t199t)1 hthd,,, ,1 11gII I- P 9,11. 91111 1 01111

Fairfie1d IhlT I Olnd-- VI d ye 1 ,n 1-91-r 9 11111 TheO 91111s1xtrt

111,9 md 9,1 h s,1l 11 9 W-- il0 1y n Oe .a M1 ,el 9 l 0 es1 n m 'e

1111 II yi 911L99 n911111 t 0099 0l eatuir- 1 1




1a11i .- I eI I. ab ou t .-1 I1 ]~ -1 1n 1 aa w h b


IIIe Nar, itn Colmbia County ThI S-t 171 R-ve dh~ppear -d low
Sntra I'I Rie ne s ch annel n tiI
pointsof dCtppea9 acn and 9appe 1an 1 The rIver fl.ws m hls channel
at tIme If -ey h~ig wae

At Thomas 1-rm m northern Gdchnst County, an ammblage .1
Mionne and Phso~nn terrestrial vertebrate remains were found mo tie chyey
i.- 909,9 ph 10 __ -t, 1111011 01111 19111 ,9 0 I yi
1nds o, the Al111c1 ua 1 o1maon Tis 1 IIes a good Indit9on 0 ta9 at 0east9
parts of thie OcaLa High area wre above ma level during Mloane time and
were emg surrounded by an inll t the marie sediments The. aras

.y veencn nnected It-irm a smaI pI nsuhi which jo ed t, larger

M 1o9 1 n -Phce0 eP9 t t1 ston a sasgres1 d hO usI .111 t0ea -1

the elevated Mioene adaments with the formation ol shorelimes and oftdioie


tins process The core b- the ridge Is ompowd of Mto -ne wdtmets, whicl
were probably deposited an a coastal lagoon or brackeslh rwer The Western
Vallc, and Guit CoastlM low]nds pro mbly are boundaries to tilts feature
M car Miocene As I me progresed the surrounding limestone plums



Lr Imestone pulrr in, opernon are or 0v e,i Ptil-eceinal
11111--111 I, t1 -1101 011. 11, 1111 11 110, I 1-dip.1







were ed 9d I Iower 9 a11m on II Mt-9anth M rne 1 d omns Th r Phio.
Ple111111e -s t110 dr- ead th asan si y thesMioene lIm-eat st .M- icswr
a, t 9 1he1 a1o1 9-they 111101 1e1a1d -oI 9 11 9 tona I lo
- -ned ond h .d bar rnd ol se Iastal fea urs o



M91 11 10191 a1e 1ep9o9I1 ated by w111 us rte 1 rye1-1 I1f hh
uta lify hin-t-onmard rk ano pble phorno -a I- e mIp-etusy been
1I'0d 1-1 19'l'l99m -1- L I]ahr 1 ,ist and a1 t 1en ounies TLe a.11








ain Ibundantoo d laOcit olnea mined lono aton i 83adhrockly
Lim e,9 09oston te 9a111 9ed are,1 9 1 1re h 1ae e en 1 eistenc1me 1 n1 9
bo -dtie .eine mnhem Ison -d d Qro a
1111 ~ ~ ~ ~~~~- -,1 .I 11 19111 I19911 011-1 90111







1 ,lub n tb u e d1, 1 0l l I'd 999 9 Il9y by bl 09l9 1 1 1 T 9e 1 o- 1





1901901io, 111, 91119199,111911)9111 111111l1-



bmonpicmarel tlpsed juot roa bst 0 iCluenn Jnd aumerous somoall quares r
_dr '= .e o..... .
iedon 91, I 9oO h -ay9 1--nld 1llml 1I0 11-Y1 Ia




d 19 1 erro9ad 919 aewarimth 1ondstunrs a1

IP w119110)1 19911oe9911-11- n1 th0111919







sm eth m e as r po g te subsuocr et h ls a d rq l u 1 t
pe19 11911bbe o 1o icl 9po 1t9ae ] Td w9ithin t heo1 lypey 9nd 9

.,,,,I' Il.lgll .91911191191lt it P

_he b i i-the'unconfmedaqln which nothas er po ton t fiea area the
1-1910.-I 11t PIAId 991.d1 lI 11, I,99911 1 111
111 111 -d1 11199

991111 ll,111110199., 91119111
demopohe re deropg bured nd poe exa s olemb pors ate contdmaqg method
eald o h e d red r o us aI th




rea aTheeA~. I Irmsanell tc i r o psts c cn wtd n ier n~ b y rmgn c n ty~ ut
hl/ g lnd- nl s yrom ,Ill n ma d A deua onlut ers dotnhro c L nevy I







ampforidan unontupeam ne~ as tow e sutbrn m 88nd hmsard croc



throuphae wJ rlz ned n ear w D icrlo imetne an9 Altougl em te atus


(leard erock b ph tlhae milta nn nd oex wtensvl thereo h tih e preent tiympernos
powphrl bmg dmentd m the mapo wate ers m eowRda
en g d 9 un11o o- 0 e11 m 1 d9 m1ned o-oy11 andt 1111, 1.






.......1 1t 9 11b9t Ir1eguate y 99er mthol 11 d me, -andr011cneov
hmonle ae C~~ose It west e t nll- n -It it ornl to loca birit ces









t 9 u 1m te ordcon o e -o1,tnr s- 1 t111
.O)i th1n -- h d t o 1tern u11 fo the flurary In bIte9

n water 1, the1 d-u-sr 11 .1 -,r 1 the 1o11n 19 t 1ont

-o -d 1 -9i I- 1in ll s. e aI Ied It w -ahe 11119 9e
099 bI 1,11111-1099 .1- Th -111111 1-9991 -1119
If1 t1a0, ro-e the 1911 o911 1- l 0 nder t199 -1,11111
of ph lravlt h towar p Iate p- ,llg p.-, -I sprng wets dlae Td
med rn hih -nprssbufaewtrI ald anI aqurr abd ,h e s defined-



A -1 n t 1a 9e l th, a11I 1 1p ,9 91,11ied -II. to1, 11 .els 9 s f e,
ai. h n nf9ind1111 quifer, 9hI9h t I- be1 1 91h111 eII 1 0111 lhd
a Tmosphee tI h oe 1,1 -- -g spa' it o e hn qi

Anther I p I- f -l s d aqi19 r- w1 hh t, n 11 1-1 t1d b101
p191 y Iayey ind, an dy ,hays, -n1 s cnded .. -nhn1d
9 19 9 hee r n d by -, I, 991 9 t e tpe Id 9 -1
A..he good --rc It grond Ite -n III, -. e ist, e ],I eonda-
alte- aquld" Ti* n" e .S retictd t. the ldgh ind res A Ies
i-pot-- -n-n.nd dqinil,, e ist n the sutl-la -n deport ot fe a
aa Ti ', n s1 temed J, -11at 11r I1.01 1au nd t ore 09119n 119r
Iit un-delin by 1Ie 1-ae -dd .r .ndy hly, oft,, highad u
The I -eden Aquiferts I, m- -d primaily ofpereal hd to,
-h, dolom .1 o-f1 T I,age. In t9 nr1,1 e1ster .1 p n h ma II

:1-dIon A110e I, uder -- ,onditionsI -od e-eh .
reai e.y Impermeabl, 1lye t 101ent9 andth -1 t It IheI west
_9p 9r 11 I t9b19 condit1ons, Th1 Ilo1 dan II i 9 I- ehag

through 1-1-11ed 10911110 hIet1one1 -nd d 9l11te tt III0
sur-ace or9a1e -19, 19ne 99 by 9 1-hiay,9 ,1 ..d. Th9 Fl11dan A1uif-9
-] eevs ehrel ro stale perchd aqier lkes, and II-am ,h-r
th, imemal di-nl, supoti gt th-e -d-,re -Iv -ee brechdd
A-owm dowwad -1r-ao .1 1-,e Another -etho If recarg t.
the Iqu-, I, by dh inll Ito Pe truh t~he -~lly I~perIous
o-dy'mg -mets it h ao ae nguti [el, Rechag,


-pg, n,. I-ivr and up-ad over.lying -,ay aufr
The IIsIl- .ids mt wate frmt.. I pe p- r -1 t the 1-1-ortda Aquife m
III ..p Ie ae rdomatb --tu and -anamb--te Ind

,b-u 1000 parts lay r-e
The -e d. y artsia aqifers" -e -Id w llu the blyey n

Icu wtm th d-whr Io ato n 1h fo o thin dis-ont-.,u
-~soe olmtmd -11 s 1e 1, bes hitch -srruded by reGti-eb
i dire-l clyyd ady cla. '

-,b,,e I lowe -ha th Itble I tII ovelyting Id-mnt. it ...rcev
rechge fro. tdoe The ..ond~y artean aqifers IIIe II Ieh -edfo

FIo. dn i, hill", Iha the -Gento ctt sufc f thInI r atm


rlra lwrtihan that If t da- te theI pele d aquW.,




moedist-ed sohds.


a TI, -1 1, wh1 Iu n19 II Ind de, 01)01
ae pr-910 pri0rily 91 1 1191 9 .1 111e -p -Th9 w1-1 It a

Seupw ou1 per Tol n tion rom o111 1 r aqA s wi he 1r p ,lent metr qsa rates





990f 9g911 1hamon -h 9, 19.b A 9 ro 9loine 119i0 111 10,1 ed p1ayt
repagin o under-lyilg aquders when d te potent-omet cle sura of thl
underlying aquters s lower than 1he water table o the su-tecl and

atmosphere by ev1po-transp ration The quaL. y e 1 11the water wun
a11,11,0 a- 19 11 1. 1 I_ 1ids109

OUTCROPS OF INTEREST


1 Levy County Township 14S, Range 16E, Section 28 Northeast quarter
of Northeast quarterI DIte L-me & Stone Compny quarry 12 m-les -utl
Iammock on U S. 19. A sity dolomtte -wr ..t-edded t
reain and I -y hd id.. dolomite re d _h _ibot
of 1tliw1 1posu11 s ar-e rom the Avon Park Nime tone
2 CIu Counyl Townlp 17S. Range 16L. Section 11 Norths quarter
of Southeast quarter, Dohme quarry ust uh 1 Barge Canal on Us 19

Dolome nodules, 9 t1e crystals and e ds are abundant m excavated




99191 011111 d m e knd 1111 1te 119hi 9s locale 1t I 1 1 Uper
4 Uii C11ount Townshlp IS, Range 181, Secion 9 No thwes9 qte
oI Southwest quarter, 9 t1r9 a br 1dge on 1 214h1. 919 r, m10 rt
nterms a anatral bade w hisil_ t 79l A --nellwe1t1g oa lormed by

5 TUyon Count-y Townshnp 8S, Range 101, Setion 3, Northwest qu-
fl Northeast quarter, Iust oI Highway 5] at Stemhatche i ells A dolonnic
lens mlormally called tIh "Stemhatchee Dolomite Membr" .1 t0, Ocala
Group is expend m fie riveI bed and banks


REFERENCES

Clark. W Mlsg R. I Mcnkc. C G, Id Ca1 .1 11, 1964,

horinda I'lorida Geological Survey Report ol Investigation No 35,
170 p
,rard, 9 w, Jr, 1968. T 'he 9,olo oj TAU he a1 h 1-6. 647 dane
li huna C( oiiur Florar Masters Thesis$ Unlvrsny of I lorda. in




M 19is A 99, 9 ,9 I -d 9 1i,7 1 i 71 dilon Tle



Pur II S Yon J Ve Rnd Oe]9sby. 9 CW R. -,, / the,/ and ,1 rtI-,





.ll....r art I ti or dan Aqufler Flori Fld Florida Bi a ofI
P Ing1), 1 MapSei s No 14
9e5non R 1O 15 l1 ) ,-lo-l1' d e, 33 C 1156
",g-dgIal S1l9-91 B0IIhn 0 N. 33, 256 p
0111 9). 1 91970- The ho e e ra11 IIt Io
0)Iu .91 Gclg) B1k1t N. 51 164 1 9


F:


1117 1111


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