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StoneLake
CR 1000 W
CR 750 N
120
5
80 90
CR 500 N
CR 400 W
Pigeon River
CR 700 N
North Twin Lake
PigeonLake
SouthTwin Lake
Scott
Seyberts
Twin Lakes
Fawn River Fawn River
CedarLake
CR 10
0 E
CR 400 N
Pigeon River Fish And
Wildlife Area
9
Ontario
Howe
80 90
CR 70
0 E
CR 400 N
CR 600 N
CR 750 N
CR 90
0 E
Brighton
3
Fawn River
Wall Lake
CR 11
00 E
80
120
GreenfieldMills
90
T . 38 N.T . 37 N.
CR 75
0 E
Pigeon RiverFish and Wildlife Area
Mongo Reservoir
20Brushy Prairie
Mongo
Pigeon River
East Fly Creek
CR 60
0 E
CR 20
0 E
CR 100 N
PlatoLaGrange
Buck Creek
CR 300 N
9
Shipshewana
ShipshewanaLake
CR 100 N
CR 700 W
20
Cass Lake
CR 1100 W
Little Elkhart River
T . 38 N.T . 37 N.
Emma Creek
CR 900 W
CR 300 S
5
T . 37 N.T . 36 N.
Rowe-Eden Ditch
CR 200 S
CR 400 S
Emma
Emma Lake
CR 100 S
CR 30
0 E
Fish Lake
Co un ty R o a d 300 S
Valentine
East Buck C reek
Fly Creek CR 200 S
Little Turkey Lake
CR 400 S
Mt.Pisgah
Elmira
3
Big Turkey
Lake
Stroh
T . 37 N.T . 36 N.
Blackman Lake
CR 90
0 E
CR 600 S Big Long
Lake
Pretty Lake
SouthMilford
3
T . 36 N.T . 35 N.
R . 11 E. R . 12 E.R . 10 E. R . 11 E.
Nauvoo Lake
Witmer Lake
Atwood Lake
Olin Lake Nature Preserve
Adams Lake
Eddy
9
Woodruff
Oliver Lake
Dallas Lake
Olin Lake
Wolcottville
R . 9 E. R . 10 E.
CR 300 W
Topeka
CR 400 W
CR 500 W
R . 8 E. R . 9 E.
CR 700 S
CR 700 W
CR 600 S
Honeyville
5
CR 1125 W
R . 7 E. R . 8 E.
T . 36 N.T . 35 N.
Scott Mill PondPublic Fishing Area
950
900
840
850
880
89090
0
830
840
850 860
870 900
910
920
950
910
920
930
940
930
R . 11 E. R . 12 E.R . 10 E. R . 11 E.
R . 9 E. R . 10 E.R . 8 E. R . 9 E.
R . 7 E. R . 8 E.
910900
920
930
940
Lake of the Woods
North
Bran
chElk
hart R
iver
7
98
1
7
7
4
3
8
2
2
6
5
8
54
9
6
2
8
11
9
9
9
56
98
7
9
3
4
8
4
98
3
1
3
2
5
2
23
4
5
4
8
3
45
1
2 1
5
6
6
1
7
13
7
6
7
23
7
5 46
6
13
24
1111
11
11 11
13
12
11
11
25
11
33
35
36
23
17
28
10
21
24
32
36
25
33
18
22
16
18
13
15
20
27
20
12
13
34
13
15
14
30
15
14
29
23
36
2825
27
21
24
13
28
24
26
16
34
35
21
24
35 36
32
26
10
33
15
20
34
19
26
12
16
16
15
18
32
2729
33
27
28
16
27
14
21
28
32 35
31
22
25
35
2826
21
25
34
29
15
32
29
17
10
23
22
25
32
29
21
14
33
19
36
27
28
23
33
16
17
25
17
33
21
16
30
27
32
17
23
23
29
21
31
16
17
23
10
3436
27
19
23
21
26
33
23
28
28
15
20
22
15
27
14
27
10
14
26
24
35
28
34
26
20
32
22
33
14
14
20
26
25
22
22
12
28
35
29
25
31
16
35
21
26
36
2324
34
30
35
12
36
26
16
3333
20
16
34
3332
22 23
13
34
36
29
35
10
29
32
20
20
2022
21
36
26
14
25
34
17
21
24
17
22
34
35
14
28
15
14
19
16
29
26
12
17
32
29
10
27
25
34
25
22
14
24
30
12
31
17
27
30
15
31
35
2423
20
24
32
13
31
24
36
36
15
19
13
18
30
29
13
13
17
12
10
22
18
19
20
17
18
31
15
19
31
18
31
18
19
13
30
19
30
30
18
18
30
31
18
19
31
18
31
19
30
30
19
7 8 9 10711 12
900
880
890
870
920
910
860850
840
830
930
820
940
950
960
970
810
960
930
940
930
920
900
930
910
950
820
940
870
910
950
960
Hillshade Map of LaGrange County, Indiana
Map gen erated b y S c o tt H. Dea nIDNR , Divisio n o f Water, R eso urc e Assessm en t S ec tio n
Divisio n o f Water Po ten tio m etric S urfac e Map 04-AMitc hell E. Da n iels, Jr., Go vern o rDepartm en t o f Natural R eso urc es
R o b ert E. Ca rter Jr., Direc to r
POT ENT IOMET R IC S UR FACE MAP OF T HE UNCONS OLIDAT ED AQUIFER S OF LAGR ANGE COUNT Y , INDIANA
Location Map
T his m ap was c reated fro m several existin g shapefiles. T o wn ship an d R an ge Lin es o f In dian a (lin e shapefile, 20020621), Lan d S urvey Lin es o f In dian a (po lygo n shapefile, 20020621), an d Co un ty Bo un daries o f In dian a (po lygo n shapefile, 20020621), were all fro m the In dian a Geo lo gic al S urvey an d b ased o n a 1:24,000 sc ale. Draft ro ad shapefiles, S ystem 1 an d S ystem 2 (lin e shapefiles, 2003), were fro m the In dian a Departm en t o f T ran spo rtatio n an d b ased o n a 1:24,000 sc ale. Po pulated Areas in In dian a 2000 (po lygo n shapefile, 20021000) was fro m the U.S . Cen sus Bureau an d b ased o n a 1:100,000 sc ale. Hydro graphy, S tream s (NHD) (lin e shapefile, 20081218), R ivers (NHD) (po lygo n shapefile, 20081218), Lakes (NHD) (po lygo n shapefile, 20081218) was fro m the U.S . Geo lo gic al S urvey an d the U.S . En viro n m en tal Pro tec tio n Agen c y an d b ased o n a 1:24,000 sc ale. Man aged Lan ds IDNR IN (po lygo n shapefile, 20100920) was fro m IDNR an d b ased o n a 1:24,000 sc ale. Co un ty Hillshade im age was fro m the U.S . Geo lo gic al S urvey Natio n al Elevatio n Dataset (raster im age, 20100324). Po ten tio m etric S urfac e Map o f the Un c o n so lidated Aquifers o f LaGran ge Co un ty, In dian a (lin e shapefiles, Gro ve, 2012) was b ased o n a 1:24,000 sc ale.
Map Use and Disclaimer StatementWe request that the fo llo win g agen c y b e ac kn o wledged in pro duc ts derived fro m this m ap: In dia n a Departm en t o f Natura l R eso urc es, Divisio n o f Water.T his m ap was c o m piled b y staff o f the In dia n a Departm en t o f Natural R eso urc es, Divisio n o f Water usin g da ta b elieved to b e reaso n a b ly ac c ura te. Ho wever, a degree o f erro r is in heren t in all m aps. T his pro duc t is distrib uted “as is” witho ut warran ties o f an y kin d, either expressed o r im plied. T his m ap is in ten ded fo r use o n ly a t the pub lished sc ale.
Potentiometric Surface Map of the Unconsolidated Aquifers of LaGrange County, Indiana
b yGlen n E. Gro ve
Divisio n o f Water, R eso urc e Assessm en t S ec tio n
Feb ruary 2012
LaGran ge Co un ty, In dia n a is lo c ated in the n o rtheastern po rtio n o f the state an d is situated en tirely within the S t. Jo seph R iver Basin . Majo r drain age system s in c lude the Pigeo n R iver, Fawn R iver an d the Little Elkhart R iver alo n g with several trib utaries. T he Po ten tio m etric S urfac e Map (PS M) o f the Un co n so lidated Aquifers o f LaGran ge Co un ty was m apped b y c o n to urin g the elevatio n s o f appro xim ately 4400 static water-levels repo rted o n well reco rds rec eived o ver a 50 year perio d. T hese wells are co m pleted in aquifers at vario us depths, an d typically, un der c o n fin ed c o n ditio n s (b o un ded b y im perm eab le layers ab o ve an d b elo w the water b earin g fo rm atio n ). Ho wever, so m e wells were c o m pleted un der un co n fin ed (n o t b o un ded b y im perm ea b le layers) settin gs. T he po ten tio m etric surfac e is a m easure o f the pressure o n water in a water b earin g fo rm atio n . Water in a n un c o n fin ed aquifer is at atm o spheric pressure an d will n o t rise in a well a b o ve the to p o f the water b earin g fo rm atio n , in c o n trast to water in a c o n fin ed aquifer which is un der hydro static pressure an d will rise in a well a b o ve the to p o f the water b earin g fo rm atio n . S tatic water-level m easurem en ts in in dividual wells used to co n struct c o un ty PS M’s are in dic ative o f the water-level at the tim e o f well co m pletio n . T he gro un dwater level within a n aquifer c o n stan tly fluc tuates in respo n se to rain fall, evapo tran spiratio n , gro un dwater m o vem en t, an d gro un dwater pum page. T herefo re, curren t site spec ific co n ditio n s m ay differ due to lo cal o r seaso n al variatio n s in m easured static water-levels. Because fluc tuatio n s in gro un dwater are typic ally sm all, static water-levels c an b e used to co n struct a gen eralized PS M. Gro un dwater flo w is n aturally fro m areas o f rec harge to ward areas o f discharge. As a gen eral rule, b ut c ertain ly n o t always, gro un dwater flo w appro xim ates the o verlyin g to po graphy an d in tersects the la n d surfa ce at m ajo r stream s. T he o b jec tive in c reatin g c o un ty PS M's is to m ap static water-levels in the upper 100 feet o f un co n so lidated m aterials. If a sec tio n o f a co un ty has few lo c ated wells within the 100 feet in terval, then the static water-levels in wells c o m pleted b etween 100 to 200 feet, if availa b le, are used to co m plem en t the area. Lo catio n al Un iversal T ran sverse Merc ato r (UT M) c o o rdin ates were either physic ally o b tain ed in the field, determ in ed thro ugh address geo co din g, o r repo rted o n water well reco rds; ho wever, the well lo c atio n fo r the m ajo rity o f the water well reco rds used to m ake the PS M were field verified. Elevatio n data were either o b tain ed fro m to po graphic m aps o r a digital elevatio n m o del. Quality c o n tro l/quality assuran c e pro c edures were utilized to refin e o r rem o ve data where erro rs were readily apparen t. Po ten tio m etric surfac e c o n to ur elevatio n s in LaGran ge Co un ty ran ge fro m a high o f appro xim ately 970 feet m ea n sea level (m sl) in the so utheast po rtio n o f the c o un ty, to a lo w o f a b o ut 810 feet m sl in the n o rthwestern c o rn er. Gen eralized gro un dwater flo w directio n appears to b e to the west-n o rthwest in the western an d n o rtheastern po rtio n s o f the c o un ty, an d to the n o rtheast an d so uthwest o ff o f a gro un dwater high in the so utheastern part o f the co un ty. T he c o un ty PS M c an b e used to defin e the regio n al gro un dwater flo w path an d to iden tify sign ifica n t areas o f gro un dwater rec harge an d disc harge. Co un ty PSM’s are in ten ded to represen t o verall regio n al c hara cteristic s an d n o t in ten ded to b e a sub stitute fo r site-spec ific studies.
1 0 10.5 Mile
1 0 10.5 K ilo m eter
Lin e o f equal elevatio n , in feet ab o ve m ean sea levelPo ten tio m etric Co n to ur in terval 10 feet
EXPLANATION
Lake & R iver
Mun ic ipal Bo un dary
US Highway
Co un ty R o ad
S tream
S tate Ma n aged Pro perty
950
In terstate
S tate R o a d
20
9
80