u.s. department of the interior prepared in cooperation ... · of 52.84 inches (southwest florida...
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P
PP
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Ona
Tampa
Ocala
Venus
DeLand
Venice
Bartow
Ruskin
Brandon
Parrish
Palatka
Tavares
Orlando
Seville
Placida
Dunedin
Bronson
Gardner
Arcadia
Sebring
Sarasota
Lorraine
Bushnell
Oklawaha
Leesburg
Lakeland
Mulberry
Pineland
Suwannee
Palmdale
La Belle
Basinger
Wauchula
Englewood
Bradenton
Chiefland
Inverness
Homosassa
Kissimmee
Polk City
Davenport
Dade City
Avon Park
Fort Myers
Clearwater
Cross City
Fort McCoy
Rock Ridge
Plant City
Fort Ogden
Frostproof
Lake Wales
Fort Meade
Cape Coral
Punta Gorda
Myakka Head
Myakka City
Saint Cloud
Lake AlfredCitrus Park
Zephyrhills
San Antonio
Brooksville
Port Richey
Gainesville
Lake Placid
Winter Haven
Daytona Beach
Fort Lonesome
Crystal River
Tarpon Springs
Port Charlotte
St. Petersburg
Altamonte Springs
30
40
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30
70
10
60
50
80
90
100
110
120
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2010
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106 113105
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STARKEY
DUNEDIN
CROSS BARRANCH
BELLEAIR
CYPRESS CREEK
MORRISBRIDGE
SOUTH CENTRAL
NW HILLSBOROUGH DISPERSED
EASTLAKE
VERNA
ELDRIDGEWILDE
NORTHPASCO
ODESSACOSME
SOUTH PASCO
LAKELAND
SECTION 21
PIN
E ISLA
ND
SO
UN
D
CHAR LO TTE
H
AR
BO
R
CALOOSAHATCHEERIVER
LAKEOKEECHOBEE
Shell
Creek
Prairie
Creek
Hor
se C
reek
Peac
e Ri
ver
Big
Slo
ugh
Cana
l
Dee
r P
rair
ie
Creek
Myakka River
LAKEISTOKPOGA
LakeJackson
LakePlacid
Lake Junein Winter
Braden River
Manatee
River
Little Manatee River
S. Prong
ReedyLake
LakeLivingston
LakeClinch
CrookedLake
BuffumLake
Peace R
i ver
LakeArbuckle
LakeWechyokapka
LakeRosalie
TigerLake
LAKE KISSIMM
EE
Lake Marian
TAMPA
BAY
HILLSB
ORO
UG
H
BAY
OLD TAMPABAY
Alafia
RiverN. P
rong
LakeHancock
LakeGarfield
LakePierce
LakeJackson
CypressLake
LakeGentry
AlligatorLake
LakePreston
East LakeTohopekaliga
LakeHart
Lake Tohopekaliga
LakeConway
LakeHamilton
LakeMarion
LakeJuliana
LakeMattie
LakeParker
LakeThonoiosassa
Blackwater
Creek
Rive
r
Hillsborough
Withlacooch
ee
River
LakeTarpon
An c l ote
River
Pithlachascoiee
River
CrewsLake
LakeMonroe
LakeJessup
LakeHarney
LAKEAPOPKA
LAKEHARRIS
LakeDora
LakeGriffin
LakeEustis
LakeDorr
LakeNorris
LakeWeir
LakePanasoffkee
Wek
iva
River
LakeLouisa
LakeMinnehaha
TSALA
APOPKA
LAKE
Crystal RiverSprings Group
LAKEGEORGE
LakeWoodruff
LakeDisston
LakeKerr
ST. JOHNS RIVER
Oklaw
aha
River
OrangeLake
LakeStafford
CRESCENTLAKE
LochloosaLake
NewmansLake
ST.
JOHNS RIVER
Wekiva
River
Riv
er
Wa
ccas
assa
GU
LF
OF
M
EX
IC
O
ATLAN
TIC O
CEA
N
LithiaSprings
SulphurSprings
RainbowSprings
HomosassaSprings
WeekiWacheeSprings
WarmMineralSprings
ChassahowitzkaSprings
CrystalSprings
L E E
P O L K
L A K E
D I X I E
TAYLOR
H E N D R Y
G L A D E S
O R A N G E
C I T R U S
M A R I O N
P U T N A M
D E S O T O
O S C E O L A
V O L U S I A
F L A G L E R
A L A C H U A
S A R A S O T A
S E M I N O L E
S T J O H N S
C H A R L O T T E
H I G H L A N D S
G I L C H R I S T
O K E E C H O B E E
P A S C O
H A R D E E
S U M T E R
M A N A T E E
P I N E L L A S
H E R N A N D O
H I L L S B O R O U G H
L E V Y
81°
81°
82°
82°
83°
83°
84°
84°
29°
29°
28°
28°
27°
27°
SCALE 1:500,000MILES
KILOMETERS
5 0 5 10 15 20
5 0 5 10 15 20
HYDROLOGIC CONDITIONS IN WEST-CENTRAL FLORIDA
The Floridan aquifer system consists of the Upper and Lower Floridan aquifers separated by the middle confining unit. The middle confining unit and the Lower Floridan aquifer in west-central Florida generally contain highly mineralized water. The water-bearing units containing fresh water are herein referred to as the Upper Floridan aquifer. The Upper Floridan aquifer is the principal source of water in the Southwest Florida Water Management District and is used for major public supply, domestic use, irrigation, and brackish water desalination in coastal communities (Southwest Florida Water Management District, 2000). This map report shows the potentiometric surface of the Upper Floridan aquifer measured in May 2007. The potentiometric surface is an imaginary surface connecting points of equal altitude to which water will rise in tightly-cased wells that tap a confined aquifer system (Lohman, 1979). This map represents water-level conditions near the end of the dry season, when ground-water levels usually are at an annual low and withdrawals for agricultural use typically are high. The cumulative average rainfall of 41.21 inches for west-central Florida (from June 2006 through May 2007) was 11.63 inches below the historical cumulative average of 52.84 inches (Southwest Florida Water Management District, 2007). Historical cumulative averages are calculated from regional rainfall summary reports (1915 to most recent complete calendar year) and are updated monthly by the Southwest Florida Water Management District. This report, prepared by the U.S. Geological Survey in cooperation with the Southwest Florida Water Management District, is part of a semi-annual series of Upper Floridan aquifer potentiometric-surface map reports for west-central Florida. Potentiometric-surface maps have been prepared for January 1964, May 1969, May 1971, May 1973, May 1974, and for each May and September since 1975. Water-level data are collected in May and September each year to show the approximate annual low and high water-level conditions, respectively. Most of the water-level data for this map were collected by the U.S. Geological Survey during the period May 21-25, 2007. Supplemental water-level data were collected by other agencies and companies. A corresponding potentiometric-surface map was prepared for areas east and north of the Southwest Florida Water Management District boundary by the U.S. Geological Survey office in Orlando, Florida (Kinnaman and Dixon, 2007). Most water-level measurements were made during a 5-day period; therefore, measurements do not represent a "snapshot" of conditions at a specific time, nor do they necessarily coincide with the seasonal low water-level condition.
WATER-LEVEL CHANGES
Water levels in about 71 percent of the wells measured in May 2007 were lower than the May 2006 water levels (Ortiz, 2007). Data from 399 wells indicate the May 2007 water levels ranged from about 21 feet below to about 8 feet above the May 2006 water levels (fig. 1). Significant water level declines occurred in north-central Pasco County and south-central Hernando County. The largest water level rises occurred in the southern half of Hardee County (fig. 1). Water levels in about 98 percent of the wells measured in May 2007 were lower than the September 2006 water levels (Ortiz, 2007). Data from 404 wells indicate the May 2007 water levels ranged from about 42 feet below to 7 feet above the September 2006 water levels. The largest water level decline was in north-central Manatee County and the largest rise in water levels was in south-central Sarasota County.
ACKNOWLEDGMENTS
The author thanks Tampa Bay Water and CF Industries for their assistance with the collection of data used to prepare this report. SELECTED REFERENCES
Kinnaman, S.L. and Dixon, J.F., 2007, Potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 2007: U.S. Geological Survey Open-File Report 2007-1371, 1 sheet.
Lohman, S. W., 1979, Ground-water hydraulics: U. S. Geological Survey Professional Paper 708, 72 p.
Ortiz, A.G., 2007, Potentiometric surface of the Upper Floridan aquifer, west-central Florida, May 2006: U.S. Geological Survey Open-File Report 2007-1032, 1 sheet.
Ortiz, A.G., 2007, Potentiometric surface of the Upper Floridan aquifer, west-central Florida, September 2006: U.S. Geological Survey Open-File Report 2007-1228, 1 sheet.
Southwest Florida Water Management District, 2000, Aquifer characteristics within the Southwest Florida Water Management District: Broooksville, Fla., 123 p.
Southwest Florida Water Management District, 2007, Hydrologic conditions for the month of May 2007: Broooksville, Fla., 81 p.
Figure 1. Change in potentiometric surface of the Upper Floridan aquifer from May 2006 to May 2007 in west-central Florida. Positive values indicate an increase in water-level altitudes.Negative values indicate a decrease in water-level altitudes
EXPLANATION
Change in the potentiometric surface, in feet
(Positive values indicate an increase in water-level altitudes)
5 to 9.99
>0 to 4.99
0 to -4.99
-5 to -9.99
-10 to -14.99
-15 to -19.99
<-20.00
AT
LA
NT
IC O
CEA
N
G U L F OF M
EX
I CO
STUDY AREA
MAP AREA
ALABAMA GEORGIA
FLORIDA
U.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY
Prepared in cooperation with theSOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT Open-File Report 2007-1380
POTENTIOMETRIC SURFACE OF THE UPPER FLORIDAN AQUIFER,WEST-CENTRAL FLORIDA, MAY 2007
By A.G. Ortiz
Base from Southwest Florida Water Management District digital data, 1992,State Plane Florida East projection, NAD83
Copies of this map can be purchased from:U.S. Geological SurveyBranch of Information ServicesBox 25286Denver, Colorodo 80225-0286
EXPLANATION
MUNICIPAL WELL FIELD
POTENTIOMETRIC CONTOUR -- Shows altitude at which water would have stood in tightly cased wells. Contour interval is 10 feet. National Geodetic Vertical Datum (NGVD) of 1929. Hachures indicate depressions. Dashed where approximately located.
BOUNDARY OF SOUTHWEST FLORIDA WATER MANAGEMENT DISTRICT
OBSERVATION WELL -- Number is altitude of water level in feet above or below NGVD of 1929.
SPRING
" CITY OR TOWN
OBSERVATION WELL -- Number is altitude of water level in feet above or below NGVD of 1929. Italic number indicates water levels corrected for salinity.
NOTE: The potentiometric contours are generalized to synoptically portray the head in a dynamic hydrologic system, taking due account of thevariations in hydrogeologic conditions, such as differing depths of wells, nonsimultaneous measurements of water levels, variable effects ofpumping, and changing climatic influence. The potentiometric contours may not conform exactly with the individual measurements of water level.
VERNA
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