GROUND WATER IN NORTH-CENTRAL TENNESSEE

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Typical wells in Houston County, Tenn. [No. 139 dug and drilled; others driHed] Depth to which well is cased (feet) Diameter of well (inches) Depth of well (feet) Approximatealtitude above sea level (feet) Topographic situation Owner or lessee Location with referencelto nearest post office No. on Plate 4 30 112 57 112 1,001 565 6 4 4 8 6 6 160(?) 64 93 493 730 425 515 610 525 500 Vail ey-_ ..... Plat Vail Hittside ..... ..... Vailey_ ....... ... ...... io- ___ _. . __ . Lou isville & Nashville R. R Ten A T\. Bell.... ....... ... Oar Stev Yell j H. Stokes^ _____ ____ . __ . Stewart Tennessee Erin, % mi le SW. .... ... .... ..... Erin, 4 mil Erin, % m ilesSW...-....... ....................... Erin, 9J£ m ilesSE _____ . ....................... Erin, 10M iniles SE ___ .. ____ .. ...... ... 139 140 144 145 149 151 153 Water level above or below surface (feet) Water-bearing beds Remarks Use of water Temperature (°F.) Yield (gallons a minute) Method of lift Depth below surface (feet) No. on Plate* Geologic horizon Character of material Public well at Stewart station. Dug well 6 feet in diameter and 30 feet deep to top of rock, with drilled hole 4 inches in diameter drilled to total depth, 57 feet. Fails in extreme drought. Other supplies of community are obtained from cisterns and dug wells about 20 feet deep. Test wen by Erin Oil & Gas Co. Small yield of water at depth of 14 feet; no water-bearing beds below depth of 177 feet. Sulphur water. Top of Chattanooga shale at depth of 370 feet. 60 3 -30 St. Louis (?) limestone. Near bottom. 139 ... -do.. ... 58 3-5 ..... do.- Cherty residuum above St. Louis limestone. Fort Payne formation. ... -do.. ... do ....... ... Fort Payne (?) formation. Fort Payne formation. do-- 140 None... _ None _ ... __ ... -20 Solution crevice .... 177 144 ... -do.. Domestic, stock.. . .....do _ , 300± 145 57 68 3 ... 3-5 .....do __ ___ No water-bearing beds below depth of 23 feet. 62 -20 Bedding-plane crevice, do 48 23 "149 151 153 1 See analysis, pp. 112-113.
to Geologic formation Typographic situation Name Owner Location with reference to nearest post office No. on Plate 4 1 Approximate altitude above sea level (feet) St. Louis or Warsaw limestone. g Do. o St. Louis limestone. ^t Fort Payne formation. ?! Do. !> Do. g St. Louis or Warsaw limestone. H Fort Payne (1) formation. W M 460 530 455 415 450 515 555 495 Valle . d Hillsi dp. Valle (3 O ...-do. ._-___ Valle y head _ VaUe y. ....... McAskill Spring Largent Bi Theodore 1 A. J. Mitcl inni W. J. Ederd._._. ..... R. E. Cros Dewey Pel ty... ..... . A. W. Ave ritt..... ....... W. M. Adl Stewart, 1 mile W _____________ Tennessee Ridge, \ 1A miles S__ ______ Erin, % m ile W. . McKinnoi i, 4% miles SE.. Stewart, 5 4. miles S_ . . Tennessee Ridge, 5M miles S....... ...... . Erin, 5 ml es SE.......... ................ Slayden, 7 138 141 143 146 147 148 150 152 § Remarks
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PLEASE DO NOT DESTROY OB THROW AWAY
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CONTENTS Pager -Abstract.__________
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OOHTBHTS V Ground water Continued.
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ABSTRACT This report describes brie
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GBOUND WATEB IN NOBTH-CENTBAL TENNE
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INTBODUCTION Q In addition to the w
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GEOGRAPHY O exist at several locali
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GEOGRAPHY / The annual range betwee
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J? §1 ? 20 158 2 20 15 GEOGRAPHY 9
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Record lacking for 1882, 1887-88, 1
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GEOGRAPHY 13 In general there is so
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SURFACE FEATURES OF CENTRAL TENNESS
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StJBFACE FEATURES OF CENTRAL TENNES
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SURFACE FEATURES OF CENTRAL TENNESS
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STJBFACE FEATURES OF CENTRAL TENNES
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SURFACE FEATUKES OF CENTKAL TENNESS
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U. S. GEOLOGICAL SUBVEY WATEH-STJPP
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U. 8. GEOLOGICAL STJEVEY WATER-SUPP
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U. S. GEOLOGICAL SURVEY WATER-SUPPL
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to O> Stratigraphic section for nor
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Stratigraphic section for north-cen
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30 GROUND WATER IN NORTH-CENTRAL TE
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32 GEOTJND WATEE IN NOETH-CENTEAL T
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34 GEOTJND WATER IN NORTH-CENTRAL T
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TJ. S. GEOLOGICAL SURVEY WATER-SUPP
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XT. S. GEOLOGICAL SUKVEY WATER-SUPP
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52 GEOTJND WATBE IN NOETH-CBNTEAL T
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j GEOUND WATEE IN NOETH-CENTEAL TEN
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72, GROUND WATER IN NORTH-CENTRAL T
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80 GROUND WATEE IN NORTH-CENTRAL TE
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TJ. S. GEOLOGICAL SURVEY WATER-SUPP
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SPEINGS 89 blank sample of water sh
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SPRINGS ' 91 formation, which are k
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SPBINGS 93 roof above its channel i
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SPKINGS bearing channel very close
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ARTESIAN CONDITIONS 97 may be expec
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GROUND "WATER IN NORTH-CENTRAL TENN
Page 122 and 123: QUALITY OF GROUND WATER 101 of diss
Page 124 and 125: QUALIFY OF GROUND WATER 103 north-c
Page 126 and 127: QUALITY OF GROUND WATER 105 nesium
Page 128 and 129: QUALITY OF GROUND WATER 107 Temains
Page 130 and 131: QUALITY OF GROUND WATEB 109 undesir
Page 132 and 133: DATA waters in north-central Tennes
Page 134 and 135: QUALITY OF GROUND WATER in north-ce
Page 138 and 139: in north-central Tennessee Continue
Page 142 and 143: QUALITY OF GROUND WATER 121 more th
Page 144 and 145: 5 Leipers and Cat beys formations:
Page 146 and 147: CHEATHAM COUNTY 125 which are trave
Page 148 and 149: Typical wells in Cheatham County, T
Page 150 and 151: fi7 3... .... 1± .do .... .... .
Page 152 and 153: GROUND WATEB IN NOKTH-CENTBAL TENNE
Page 154 and 155: DAVIDSON COUNTY 133 have the same w
Page 156 and 157: Typical wells in Davidson County, T
Page 158 and 159: At 1400 Eighth Ave. N. At foundry,
Page 160 and 161: Typical springs in Davidson County,
Page 162 and 163: DICKBON COUNTY 141 the Highland Rim
Page 164 and 165: DICKSON COUNTY 148 mineral matter,
Page 166 and 167: Water-bearing beds Remarks Use of w
Page 168 and 169: Typical springs in Dickson County,
Page 170 and 171: HOUSTON COUNTY 149 superficial rela
Page 174 and 175: GBOUND WATEB IN NOETH-CENTEAL TENNE
Page 176 and 177: HUMPHREYS COUNTY 155 and elsewhere
Page 178 and 179: HUMPHREYS COUNTY 157 prove inadequa
Page 180 and 181: Typical wells in Humphreys County,
Page 182 and 183: Typical springs in Humphreys County
Page 184 and 185: MONTGOMERY COUNTY 163 Driller's log
Page 186 and 187: MONTGOMERY COUNTY 165 and most of t
Page 188 and 189: Maximum consumption 1,200 gallons a
Page 190 and 191: e-s §8238 o o o o o o p: S JH.-C 3
Page 192 and 193: EOBEETSON COUNTY 171 GROUND-WATER C
Page 194 and 195: Typical wells in Robertson County,
Page 196 and 197: Water turbid. Stock.. .. .........
Page 198 and 199: GROUND WATEB IN NORTH-CENTRA!, TENN
Page 200 and 201: RUTHERFORD COUNTY 179 water table a
Page 202 and 203: RUTHERFORD COUNTY 181 and passing t
Page 204 and 205: RUTHERFORD COUNTY 183 tated as the
Page 206 and 207: 6± miles E.. _ _ .. __ ._ _ ___ ..
Page 208 and 209: ..... do... ... .... 138 ....... Ne
Page 210 and 211: 58 None .............. }... .do ...
Page 212 and 213: STEWABT COUNTY 191 _ In addition to
Page 214 and 215: wash and weathered rocks in the low
Page 216 and 217: .....do....... ..... do....... Buck
Page 218 and 219: Approximate yield Openings Tempera-
Page 220 and 221: StJMNEB COUNTY 199 mately N. 70° E
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SOI hydrogen sulphide and contains
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SUMNEE COUNTY 208 Gallatin are know
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Do. hillside springs. derive water
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WILLIAMSON COUNTY Driller's log of
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WJfetlAMSON i&entf&nts, also in thf
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WILL1AMSON COUNTY 211 perennial spr
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COUNTT trated calcium bicarbonate w
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Typical wells in Williamson County,
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-130- Shale . use. beds found below
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Approximate yield Openings Remarks
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WILSON COUNTY 221 entire Middle and
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WILSON COUNTY 223 chemical characte
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WILSON COUNTY stitute the source of
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WIIJSON COUNTY 227 associated with
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WILSON COUNTY 229 pump is driven th
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* Water-bearing beds Remarks Use of
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Typical springs in Wilson County, T
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236 INDEX F Page Farrar, D. F., ana
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238 INDEX Page Sumner County, munic
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GROUND WATER IN NORTH-CENTRAL TENNESSEE

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