STATE OF FLORIDA STATE BOARD OF CONSERVATION DIVISION OF GEOLOGY WATER LEVELS IN ARTESIAN AND NONARTESIAN AQUIFERS OF FLORIDA IN 1960

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1 STATE OF FLORIDA STATE BOARD OF CONSERVATION DIVISION OF GEOLOGY FLORIDA GEOLOGICAL SURVEY Robert 0. Vernon, Director INFORMATION CIRCULAR NO. 33 WATER LEVELS IN ARTESIAN AND NONARTESIAN AQUIFERS OF FLORIDA IN 1960 By Henry G. Healy,Geologist U. S. Geological Survey Prepared by the UNITED STATES GEOLOGICAL SURVEY In cooperation with the FLORIDA GEOLOGICAL SURVEY and other STATE AND LOCAL AGENCIES TALLAHASSEE 1962

2 AGRI- CULTURAL LIBRARY Completed manuscript received July 14, 1961 Printed by the Florida Geological Survey Tallahassee, :... '*v-

3 TABLE OF CONTENTS Page Introduction... 1 ILLUSTRATIONS Figure 1 Map showing extent of principal aquifers and sources of ground-water supplies Locations of selected observation wells Hydrographs of water levels in selected wells in Florida in Table 1 Well data on selected observation wells iii

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5 WATER LEVELS IN ARTESIAN AND NONARTESIAN AQUIFERS OF FLORIDA IN 1960 By Henry G. Healy The purpose of this report is to summarize the trends and fluctuations of water levels in the principal artesian and nonartesian (water-table) ground-water reservoirs or aquifers of Florida during Adequate water supplies are essential to the continued industrial and municipal growth of the State. Since World War II, particularly during the last decade, the demand for ground water for industrial and municipal use has increased yearly in many parts of the State. At present, the demand has not exceeded the ground-water supply in most areas but the supply is limited and if the demand for water continues to increase as it has during the last decade, many areas may have ground-water shortages in the future. In order to prevent such future shortages, the present supplies must be appraised and effectively utilized. The measurement of water-level fluctuations in observation wells is an important phase in the appraisal of ground-water resources of the State. The Floridan and Biscayne aquifers are two of the most important aquifers in the State. The areal extent of these aquifers is shown in figure 1. The Floridan aquifer underlies most of the State and it is the principal source of ground water in central, northern, and most of northwestern Florida. Highly mineralized water precludes the usefulness of the Floridan aquifer as a source of potable water supply in sop~e coastalareas and most of southern Florida. In these

6 N ( 7 EXPLANATION Biscayne aquifer 0 Floridon aquifer 0 Other aqulfers FLORIDA Ie * Mlle. * Figure 1. Map showing extent of principal aquifers and sources of ground-water supplies.

7 INFORMATION CIRCULAR NO areas, the shallow nonartesian (water-table) aquifers are the chief source of ground water. The Biscayne aquifer in southern Florida is the most highly productive of the shallow nonartesian aquifers in Florida. In northwestern Florida, unconsolidated deposits of sand and gravel yield large supplies of ground water for industrial and municipal uses. The statewide observation well network is an integral part of the Federal-State cooperative program for the investigation of ground-water resources of the State. At present, the statewide network includes a total of 7Z7 observation wells in 45 of the 67 counties of the State; of these, measurements for 163 wells are published periodically in U.S. Geological Survey water-supply papers. This report presents hydrographs of water-level fluctuations in63 observation wells selected from the statewide network. Location of the selected wells are shown infigure 2. Additional waterlevel data for the wells used in this report and water-level data for all other wells in the statewide network are available from the office of the U. S. Geological Survey, Ground Water Branch, Tallahassee, Florida. Fluctuations of ground-water levels reflect changes in the quantity of water stored in an aquifer. The annual net changes of water levels during 1960, as shown by the hydrographs, show that the amount of water stored in the principal aquifers remained about the same in northern Florida, increased in central Florida, and decreased in the southern part of the State. Water levels in artesian aquifers were above average in most areas in northern, central, and southern Florida at the beginning of the year and then declined tobelow average. At the end of the year, water levels were above average in most areas in northern and central Florida, but were near or below average in most areas in southern Florida. Water levels in nonartesian aquifers were above average at the beginning of the year, and declined to near or below average in many areas during the year. At the end of the year, water levels were below average and lower than water levels at the beginning of the year in most areas in

8 4 FLORIDA GEOLOGICAL SURVEY G E 0 R G IA N r V -?,rc,,c 300r \* /^ti * M ",, Jo;-.sL - - j& \- f -r y i "^* ftt-r Pr m --n. - 1 Figure 2. Locations of selected observation wells.

9 INFORMATION CIRCULAR NO southern Florida. Net changes of water levels were essentially caused by below average rainfall during October through December. Table 1 contains the following pertinent information on the observation wells: aquifer penetrated, the depth of well, and the depth of casing. Hydrographs showing the trends and fluctuations of water levels in observation wells in the artesian and nonartesian aquifers in the State are shown in figure 3. The hydrographs show end-of-month water levels for 1960 which are compared to the maximum, minimum, and average water levels computed from end-of-month water levels for the period of record. Table 1. Well Data on Selected Observation Wells Depth Depth Well of well of casing County Number Aquifer (in feet) (in feet) Remarks Bay BA 20 Floridan Water levels affected by pumping from near - by wells Broward BR 561 Biscayne Broward BR 616 Biscayne Collier CL 54 Nonartesian 9 8 Collier CL 131 Nonartesian Columbia CO 9 Floridan Dade DA 18 Biscayne Dade DA 19 Biscayne Water levels affected by pumping Dade DA 39 Biscayne 6 6 Water levels affected by pumping Dade DA 72 Biscayne 5 4 Dade DA 179 Biscayne Dade DA 182 Biscayne Dade DA 196 Biscayne Dade DA 551 Biscayne Water levels affected by pumping Dade DA 596 Biscayne Dade DA 618 Biscayne Dade DA 620 Biscayne 16 6 Dixie DX 15 Floridan Water levels occasionally affected by pumping Duval DU 206 Floridan 1,920 1,000 Reported depth Escambia ES 45 Artesian Escambia ES 62 Artesian Escambia ES 62A Nonartesian Gulf GF 30 Floridan Water levels affected by pumping from near - by wells; reported depth

10 6 FLORIDA GEOLOGICAL SURVEY Table I. (Continued) Depth Depth Well of well of casing County Number Aquifer (in feet) (in feet) Remarks Hendry HE 3 Nonartesian 10 8 Highlands HI 9 Nonartesian Highlands HI 10 Nonartesian Highlands HI 13 Nonartesian Highlands HI 14 Nonartesian Highlands HI 15 Nonartesian Hillsborough HL 13 Floridan Hillsborough HL 30 Floridan Flowing well; reported depth Hillsborough HL 500 Floridan Water levels occasionally affected by pumping Indian River IR 25 Nonartesian Lee LE 414 Nonartesian Water levels affected by pumping from near - by wells Leon LN 36 Nonartesian Marion MA 5 Floridan Martin MN 140 Nonartesian Flowing well Martin MN 147 Nonartesian Water levels affected by pumping from near - by wells Okeechobee OK 2 Nonartesian Okeechobee OK 3 Nonartesian Osceola OS 171 Nonartesian Osceola OS 181 Nonartesian Osceola OS 183 Nonartesian Palm Beach PB 99 Biscayne Palm Beach PB 109 Nonartesian 14 9 Pasco PA 16 Floridan Pinellas PI 13 Floridan Pinellas PI 246 Floridan Pinellas PI 561 Floridan Polk PO 44 Floridan Occasionally flows Polk PO 45 Floridan Polk PO 47 Nonartesian Polk PO 49 Nonartesian Polk PO 51 Floridan Water levels affected by pumping from near - by wells St. L.cie ST.L1A Nonartesian L. Lucie ST. AZ Nonartesian Santa Rnsa SR 102 Nonartesian Sarasota SA 9 Floridan Occasionally flows Taylor TA 35 Floridan Water levels affected by pumping from near - by wells; occasionally flows Volusia VO 31 Floridan Volusia VO Floridan Occasionally flows Wakulla WA 2 Floridan Occasionally flows

11 INFORMATION CIRCULAR NO Figure 3. Hydrographs of water levels in selected wells in Florida in Explanation: Elevation in feet referred to mean sea level (MSL) or land-surface datum (LSD); solid line indicates elevations in 1960; unshaded portion shows maximum and minimum of record; broken line indicates normal (average) for period of record.

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13 INFORMATION CIRCULAR NO MILLVILLE FORT LAUDERDALE 88J F J F M A M J J A S 0 N D S108 -i j128 ; O BA20 RECORD BEGINS 1951 BR 561 RECORD BEGINS 1948 WEST OF POMPANO BIG CYPRESS SWAMP 0 J F M A M J J A S N D 20 J F MA MJ J ASO0 ND 1o 5 B 15 o 0 #"A'5~A oo4,,o...? t : BR 616 " RECORD BEGINS 1950 CL 54 RECORD BEGINS 1951 IMMOKALEE LAKE CITY 30JFMAMJJASO ND J F M A M J J A S O N D -J, " IMMCORLEEBLAKESCITY u i CL 131 RECORD BEGINS 1952 CO 9 RECORD- BEGINS 1942

14 10 FLORIDA GEOLOGICAL SURVEY OPA-LOCKA MIAMI SPRINGS 1J F M AM J J A S 0 N D 15J FMA MJ J A S ON D O-j -II w 55 DA 18 RECORD BEGINS 1940 DA 19 RECORD BEGINS 1940 D0 O SOUTH MIAMI EVERGLADES 15 J: F MA M J J A S O N D J F M A M J J A S O N D o O DA 39 RECORD BEGINS 1940 DA 72 RECORD BEGINS 1940 MIAMI PETERS J F MA M J J A S 0 N D J FM A M J J A S 0 ND -4 n." ' ' 5" >5 DA [79 RECORD BEGINS 1940 "DA 182 RECORD BEGINS 1940

15 INFORMATION CIRCULAR NO J HOMESTEAD SOUTHWEST WELL FIELD F M A M J J A S O N D J F M A M J J A S O N D V) U) ^ --, -,,^ ^ o " DA 196 RECORD BEGINS 1933 DA 551 RECORD BEGINS 1948 EVERGLADES EVERGLADES J F M A M J J A S O N D J F M A M J J A S O N D -0o ' ' o -- i.. - d. ~o -rc -- m DA 596 RECORD BEGINS 1949 DA 618 RECORD BEGINS 1951 EVERGLADES CROSS CITY J F MA M J J A S 0 N D J F M A M J J A S 0 N D m DA 620 RECORD BEGINS 1951 DX 15 RECORD BEGINS 1957

16 12 FLORIDA GEOLOGICAL SURVEY WESCONETT CANTONMENT J F MA M J.J AS O N D J FM AM J J A S 0 N D SO 92_.9 -j o o S DU 206 RECORD BEGINS ES45 RECORD BEGINS 1940 PENSACOLA PENSACOLA J F MA M J J A S 0 N D J F M A M J J A S O N D On'^ w -S - - i ^. C3 10 `V S W ES 62 RECORD BEGINS 1940 ES 62A RECORD BEGINS 1940 PORT ST JOE SEMINOLE RESERVATION J F M AM J J A S O N D J FM A M J J A S O N D TO DATE -:-:-::15,..., :..: RECORD BEGINS 1946 HE 3 RECORD ; 1950 TO DATE

17 INFORMATION CIRCULAR NO EAST OF AVON PARK SEBRING O D 135 J F M A M J J A S 0 N D 95 J... F M A.M J J A S N ~ HIS9 RECORD BEGINS 1948 HI 10 RECORD BEGINS 1948 BRIGHTON CHILDS JFMAMJJASOND JFMAMJ JASOND HI 13 RECORD BEGINS 1948 HI 14 RECORD BEGINS 1948 BRIGHTON CITRUS PARK J F M A M J J A S 0 N D J F M A M J J A S O N D HI 15 RECORD BEGINS 1948 HL 13 RECORD BEGINS '-' '" IC HI 15 RECORD BEGINS 1948 HL 13 RECORD BEGINS 1930

18 14 FLORIDA GEOLOGICAL SURVEY RUSKIN WIMAUMA 0 o 51 (n a a0 85 '56 N 61 HL 30 RECORD BEGINS 1950 HL 500 RECORD BEGINS 1951 EAST J OF J YEEHAW FORT MYERS J F M AM A S O N D J F M A M J J A S O N D a30 c20 o a IR 25 RECORD BEGINS 1950 LE 414 RECORD BEGINS 1948 J TALLAHASSEE SHARPES FERRY 0 F M A M J J AMJy- A S O N D w- o 61,.0 EGN9103 IR 2536 RECORD BEGINS 1950 LE 414 RECORD BEGINS

19 _J [ INFORMATION CIRCULAR NO WEST OF MADISON WEST OF JUPITER J F M A M J J A S O N D J F M A M J J A S 0 N D S wi 0 o30 15 " ^^, _ MD 18 RECORD BEGINS 1952 MN 140 RECORD BEGINS 1950 STUART FORT BASINGER J F M A M J J A S 0 N D J F M A M J J A S 0 N D i o 35 MN 147 RECORD BEGINS 1952 OK 2 RECORD BEGINS 1949 FORT DRUM NORTH OF DEER PARK S FMAMJ JASON D JFMAM JJ ASOND 0. w , - 0 OK 3 RECORD BEGINS i948 OS 171 RECORD BEGINS 1950

20 1 6 F.LO( JIDA GEOLOGICAL SURVEY WEST OF HOLOPAW SOUTH OF KENANSVILLE J F MAM J AS O N D J FM A M J J A S O N D (n 75 > > OS 181 RECORD BEGINS 1948 OS 183 RECORD BEGINS 1948 WEST PALM BEACH EVERGLADES J F M A M F M JFMAM J J A S 0 N D J FM A M J J A S 0 N D n PB 99 RECORD BEGINS 1948 PB 109 RECORD BEGINS 1951 ZEPHYRHILLS TARPON SPRINGS J F MA M J J A S 0 N D JF M A M J J A S O N D :::::..- ::::-., J...:" :::: S0 50 Sm PA 16 RECORD BEGINS 1936 PI 13 RECORD BEGINS 1947

21 INFORMATION CIRCULAR NO CLEARWATER NORTH OF SAWGRASS LAKE J F M AM J J A S'O N D J F M A M J J A S O N D 20. c , : X-N:,.... :$:.$ P1 246 RECORD BEGINS 1945 PI 561 RECORD BEGINS 1947 DAVENPORT SAND GULLY 5 J F M A M J J A S 0 N D J FM A M J J A S 0 N D 5 S0 X.X-X 62, DAVENPORT WEST OF LAKE KISSIMMEE J F M A M J A N D A N D 120 J S 0 J F M A M < ID 0 a PO 47 RECORD BEGINS 1948 PO 49 RECORD BEGINS 1949

22 1i FI-'.U1(R A GEOLOGICAL SURVEY FROSTPROOF EAST OF OKEECHOBEE J FM AMJ J A SO NDM A M J J A SON D u PO 51 RECORD BEGINS 1949 ST L 41 RECORD BEGINS LJ EAST OF FORT PIERCE GULF BREEZE 35J F M A M J J A SO N D J FM A M J A S 0 N D I * 4/\ t c 25 S co,, " ST L 42 RECORD BEGINS 1950 SR. 102 RECORD BEGINS 1950 ST L 42 RECORD BEGINS 1950 SR. 102 RECORD BEGINS 1950 J F M A M PALMER J J A FARMS S 0 N D J F M A M FOLEY J J A S 0 N D s., " " "..-I -10-J SA 9 RECORD BEGINS 1930 TA 35 RECORD BEGINS 1946

23 INFORMATION CIRCULAR NO ALAMANA J F M A M J 0 'A JFMAME VO 31 RECORD BEGINS 1936 EAST OF DELANO JJFMAMJJASOND 5 o F M A M N - W JFM EAST OF DELANDRKS ST. ARK 0I (: u),.. VO 31 RECORD BEGINS 1936,_. -" WA 2 RECORD BEGINS 1937

24 -FLORIDA-GEOLOGICAL-SURV COPYRIGHT NOTICE [year of publication as printed] Florida Geological Survey [source text] The Florida Geological Survey holds all rights to the source text of this electronic resource on behalf of the State of Florida. The Florida Geological Survey shall be considered the copyright holder for the text of this publication. Under the Statutes of the State of Florida (FS ; , and ), the Florida Geologic Survey (Tallahassee, FL), publisher of the Florida Geologic Survey, as a division of state government, makes its documents public (i.e., published) and extends to the state's official agencies and libraries, including the University of Florida's Smathers Libraries, rights of reproduction. The Florida Geological Survey has made its publications available to the University of Florida, on behalf of the State University System of Florida, for the purpose of digitization and Internet distribution. The Florida Geological Survey reserves all rights to its publications. All uses, excluding those made under "fair use" provisions of U.S. copyright legislation (U.S. Code, Title 17, Section 107), are restricted. Contact the Florida Geological Survey for additional information and permissions.