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Big Pine C reek
Sugar
Mud Creek
Coon Creek
Finigan D itch
Carpenter Creek
Leuck Ditch
Creek
Miller
Little
Pine
Cree
k
Brumm Ditch
Grete
ncord
Ditc
h
Darby Ditch
Kult
Upper Sugar
Harrington
Gille
n Ditc
hPine Creek Ditch
Hollingsworth
Salmon
Seam
ons D
itch
Farrell
Humbert
Lamber t
Wattles Ditch
Brown D
itch
North
Sween
eyDi
tch
Moore D itch
Lague
Prud
entia
l Ditc
h
Ella
Owens
Bartondale Ditch
Coon Creek
CR 800 N
CR 300 N
CR 200 E
CR 500 N
CR 600 E
CR 300 E
CR 200 S
CR 400 N
CR 400 E
CR 600 N
CR 500 E
CR 100 N
CR 1000 E
CR 200 W
CR 700 E
CR 300 S
CR 100 E
CR 700 N
CR 800 E
CR 800 S
CR 1100 E
CR 900 E
CR 500 S
CR 1000 W
CR 500 W
Meridian Rd
CR 600 S
CR 650 N
CR 400 W
CR 300 W
CR 100 W
CR 850 E
CR 750 E
CR 700 W
CR 100 S
CR 600 W
CR 550 N
CR 750 S
CR 975 E
CR 900 W
CR 150 S
CR 875 E
CR 700 S
CR 400 S
CR 50 W
CR 250 N
Divisio n Rd
CR 200 N
CR 725 E
CR 550 S
CR 650 S
CR 800 E
Old U S 41
CR 1150 E
CR 475 N
CR 200 E
CR 700 W
CR 1075 E
CR 200 S
CR 300 S
Divisio n Rd
CR 200 S
CR 500 W CR 100 W
CR 800 S
CR 800 W
CR 500 E
CR 700 S
CR 850 E
CR 400 W
CR 300 E
CR 500 S
CR 600 W
CR 600 ECR 100 W
CR 700 N
CR 850 S
CR 800 S
CR 400 S
CR 1100 E
CR 200 N
CR 600 N
CR 500 W
CR 400 N
CR 900 E
CR 500 N
CR 100 S
CR 750 S
CR 100 E
CR 700 W
CR 700 S
CR 150 S
CR 1000 W
CR 400 S
CR 400 W
CR 100 S
CR 200 W
£¤52
¬«18
¬«18
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¬«55
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Fowler
Earl Park
OxfordBoswell
OtterbeinAmbia
Pine CreekBottoms Gamebird
Habitat Area
Kirsch Gamebird
Habitat Area
Watland Gamebird
Habitat Area
GessweinGamebird
Habitat Area
Vinegar Hill(Codden Farm)
GamebirdHabitat Area
Jefvert Gamebird
Habitat Area
Nickle PlateFarms Wildlife
ManagementArea
Knob ViewGamebird
Habitat Area
Metro-Sixty Gamebird
Habitat Area
Brouillette (Mcginnis)Gamebird Habitat Area
Deno GamebirdHabitat Area
Falwell GamebirdHabitat Area
McGinnis/Lauerman Gamebird Habitat Area
GreenwoodDitch Gamebird
Habitat Area
Raub GamebirdHabitat Area
¬«71
¬«18
¬«71
¬«352
¬«55
680
700
710
710
720
730
740
750
730 740
750750
750
740730
Ditch
750
700720
730
770
700
690
710
720
730
740
750
770
750760
770
730
700690
680
690700
710
730
£¤41
B row n Ditch
Ditch
Ditch
Goose
Fork
Vermilion River
DitchDit ch
710
Sugar Creek
Creek
Sugar Cre e k
Creek
760
770760
770
780
770Ditch
760
750
730
710
DitchDitch
B igPin
eCree k
Mud Pine Creek
Ditch¬«55
£¤52
CR 200 E
Kankakee River Basin
Middle WabashRiver Basin
KankakeeRiver Basin
Middle WabashRiver Basin
Upper WabashRiver Basin
Raub
Sheff
Free
FreelandPark
DunnDunnington
Handy
Talbot
Chase
Templeton
Foresman
Atkinson
Swanington
Barce
Lochiel
Wadena
Gravel Hill
R. 10 W. R. 9 W.T. 27 N.T. 26 N.
R. 9 W. R. 8 W. R. 8 W. R. 7 W. R. 7 W. R. 6 W.T. 27 N.T. 26 N.
T. 26 N.T. 25 N.
T. 25 N.T. 24 N.
T. 24 N.T. 23 N.
R. 7 W. R. 6 W.R. 8 W. R. 7 W.R. 9 W. R. 8 W.R. 10 W. R. 9 W.
T. 24 N.T. 23 N.
T. 25 N.T. 24 N.
T. 26 N.T. 25 N.
£¤41
£¤52
£¤52
¬«352
Ditch
Latera
l
760
720
Divisio n o f Water Potentio m etric Surfa c e Ma p 50-BMic ha el R. Penc e, Go verno r
Dep artm ent o f Natura l Resourc esCa m ero n F. Clark, Directo r
POT ENT IOMET RIC SU RFACE MAP OF T HE BEDROCKAQU IFERS OF BENT ON COU NT Y, INDIANA
Map generated by Reub en Q. ArvinIDNR, Divisio n o f Water, Reso urc e Assessm ent Sectio n
Location Map
Hillshade Map of Benton County, Indiana
Potentiometric Surface Map of the Bedrock Aquifers of Benton County, Indiana
b yRa nd a l D. Ma ier
Divisio n o f Water, Reso urc e Assessm ent Sectio n
Ja nuary 2015
County Ro a d
U S Highwa y£¤52
State Ro a d ¬«71
EXPLANATION
Strea m
L ine o f equa l elevatio n, in feet a b o ve m ea n sea levelPotentio m etric Co ntour interva l 10 feet
L a ke & RiverNo Aquifer Materia lo r L im ited Data
Basin Bound ary
720
DNR Ma na ged L a nd s
Munic ip a l Bound ary
®1 0 10.5 Mile
1 0 10.5 Kilo m eter
T his m a p is created fro m severa l existing sha p efiles. T o wnship a nd Ra nge L ines o f Ind ia na (line sha p efile, 20020621), L a nd Survey L ines o f Ind ia na (p o lygo n sha p efile, 20020621), a nd County Bound aries o f Ind ia na (p o lygo n sha p efile, 20020621), are a ll fro m the Ind ia na Geo lo gic a l Survey a nd b ased o n a 1:24,000 sc a le. Ro a d s (T IGER a nd INDOT ) (line sha p efile, 2005) is fro m the Ind ia naDep artm ent o f T ra nsp o rtatio n a nd b ased o n a 1:100,000 sc a le. System 1 (line sha p efile, 2003) is fro m the Ind ia na Dep artm ent o fT ra nsp o rtatio n a nd b ased o n a 1:24,000 sc a le. Inc o rp o rated Bound aries in Ind ia na (p o lygo n sha p efile, 20060501) is fro m the Gra p hic s a nd Engineering Sectio n, Ind ia na Dep artm ent o f T ra nsp o rtatio n. Hydro gra p hy, Strea m s (NHD) (line sha p efile, 20081218), Rivers (NHD) (p o lygo n sha p efile, 20081218), a nd L a kes (NHD) (p o lygo n sha p efile, 20081218) are fro m the U .S. Geo lo gic a l Survey a nd b ased o n a 1:24,000 sc a le. Basin b o und a ries are m o d ified fro m Watershed Bound a ry Dataset (p o lygo n sha p efile, 2008) fro m the Natura l Resourc e Co nservatio n Servic e a nd b ased o n a 1:24,000 sc a le. Ma na ged L a nd s IDNR IN (p o lygo n sha p efile, 20100920) is fro m the Ind ia na Dep artm ent o f Natura l Resourc es a nd b ased o n a 1:24,000 sc a le. T he Hillsha d e im a ge is d erived fro m the Ind ia na Ortho/L iDAR Statewid e Co llectio n Pro gra m (2013). Bento n County Bedro c k No Aquifer Materia l or L im ited Data (p o lygo n sha p efile, Ma ier, 2015) a nd Potentio m etric Surfa c e Co ntours o f the Bedro c k Aquifers o f Bento n County, Ind ia na (line sha p efile, Ma ier, 2015) are b ased o n a 1:24,000 sc a le.
Bento n County, Ind ia na is lo c ated in the no rthwest p art o f the state a nd is within the b o und aries o f three river b asins. T he c o unty is genera lly sp lit a lo ng a no rtheast-southwest trend ing b o und ary with the no rthwestern area within the Ka nka kee River Basin a nd the southeastern p o rtio n within the Mid d le Wa b ash River Basin. Ho wever, the no rtheastern area o f the c o unty is lo c ated in the U p p er Wa b ash River Basin.T he p o tentio m etric surfa c e m a p p ed (PSM) c o ntour elevatio ns represent lines o f equa l elevatio n relative to the m easured ground water levels in wells. In genera l, wells c o m p leted in a c o nfined aquifer system are b o und by im p erm ea b le la yers a nd will ha ve static water levels und er hydrostatic pressure c ausing the water level to rise a b o ve the elevatio n o f the aquifer resourc e. In c o ntrast, a n unc o nfined aquifer system is not b o und by im p erm ea b le la yers; therefo re, the water level will no t b e und er hydrostatic pressure a nd will no t rise a b o ve the aquifer resourc e. Static water level m easurem ents in ind ivid ua l wells used to c o nstruct the p o tentio m etric surfa c e m a p are ind ic ative o f the water level at the tim e o f well c o m p letio n. T herefo re, current site sp ec ific c o nd itio ns m a y d iffer due to lo c a l or seaso na l variatio ns in m easured static water levels.Co o rd ina te lo c atio ns o f water well rec o rds were p hysic a lly o bta ined in the field , d eterm ined through a d d ress geo c o d ing, or rep o rted o n water well rec o rds. Elevatio n d ata were o bta ined fro m a d igita l elevatio n m o d el (DEM). Elevatio n a nd lo c atio n qua lity c o ntro l/qua lity assura nc e pro c ed ures were utilized to refine or rem o ve d ata where errors were rea d ily a p p arent.
Potentio m etric surfa c e elevatio ns ra nge fro m a high o f 780 feet m ea n sea level (m sl) in the c entra lp art o f the c o unty, to a lo w o f 680 feet m sl in the no rthwest c o rner o f the c o unty a nd to the southeast p art o f the c o unty a lo ng a p o rtio n o f Big Pine Creek.
In Bento n County, wells pro d uc ing fro m b ed ro c k d ep o sits are extrem ely lim ited with m uc h o f the c o unty la c king in d ata. T his is prim arily due to b ed ro c k as a lim ited aquifer resourc e, a nd /or ava ila b le o verlying unc o nso lid ated m ateria ls. T herefo re, p o tentio m etric surfa c e elevatio n c o ntours ha ve no t b een extend ed througho ut m uc h o f the c o unty.Bedro c k fo r the m a jo rity o f the c o unty inc lud es siltsto ne a nd sha le asso c iated with the Mississip p ia n Bord en Group. Alo ng the eastern ed ge o f the c o unty, bed ro c k inc lud es the Devo nia n a nd Mississip p ia n New Alb a ny Sha le. A sm a ll area a lo ng the no rth-c entra l c o unty b o und ary is sa nd sto ne a nd sha le o f the Pennsylva nia n Ra c c o o n Creek Group a nd a no ther sm a ll area a lo ng the no rtheastern c o unty b o und ary inc lud es Siluria n a nd Devo nia n c arb o nates. T here are 168 lo c ated wells that are c o m p leted in b ed ro c k a nd are utilized to wards the m a p p ing o f the b ed ro c k p o tentio m etric surfa c e. T o ta l well d ep ths genera lly ra nge fro m 31 to 435 feet with d ep ths to the b ed ro c k surfa c e at 8 to 303 feet.
Genera lized ground water flo w d irectio n fo r the c o unty is to wards m a jo r dra ina ge releva nt to the b asin. T herefo re, in the Ka nka kee River Basin ground water flo w is genera lly to the no rthwest; a nd in the Mid d le Wa b ash River Basin ground water flo w is to the south-southeast. Although no c o ntours are represented fo r the U p p er Wa b ash River Basin in Bento n County, ground water flo w is to wards the east.
Map Use and Disclaimer StatementWe request that the fo llo wing a genc y b e a c kno wled ged in pro d ucts d erived fro m this m a p : Ind ia na Dep artm ent o f Natura l Resourc es, Divisio n o f Water.T his m a p was c o m p iled by sta ff o f the Ind ia na Dep artm ent o f Natura l Resourc es, Divisio n o f Water using d a ta b elieved to b e reaso na b ly a c curate. Ho wever, a d egree o f error is inherent in a ll m a p s. T his pro d uct is d istributed “as is” witho ut warra nties o f a ny kind , either expressed or im p lied . T his m a p is intend ed fo r use o nly at the pub lished sc a le.