GROUND WATER IN NORTH-CENTRAL TENNESSEE

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QUALITY OF GROUND WATER in north-central Tennessee Continued 113 Analyses (quantities In parts per million) Total dis solved solids at 180° C. 162 4,502 214 2,236 292 385 628 262 15S 159» 161 164 ier 171 ITS 177" ISO- 190 191 198-A d Total by summation of constituents. Determinations of HjS and SO 4 by Margaret D. Foster.
114 GROUND WATER IN NORTH-CENTRAL TENNESSEE No. on Plate 4 198-B 218 219 220 225 229 243 258 259 260 265 268 269 277 278 279 282 286 292 294 295 Location and description DICKSON COUNTY continued Analyses of representative ground waters deep; water from St Louis or Warsaw limestone; W. R. Berry, owner. Sampled Oct. 7, 1927. White Bluff, ^ mile west of.' Drilled well 5% inches in diameter and 75 feet deep; water from St. Louis or Warsaw limestone; owned by Jesse Gill. Sampled Oct. 8, 1927. St. Louis or Warsaw limestone; owned by Nashville, Chattanooga & St. Louis Ry. Sampled Oct. 8, 1927. White Bluff, ^ mile south of. Drilled well 8M inches in diameter and 1,383 feet deep; water from top of Chattanooga shale at depth of 246 feet; owned by White Bluff Canning Co. Sampled Oct. 8, 1927. or Warsaw limestone; owned by city of Dickson; municipal supply. Sam pled Oct. 8, 1927. Dickson. Drilled well 5M inches in diameter and 427 feet deep; water from St. Louis or Warsaw limestone at depth of 75 feet; owned by Dickson Ice Co. Sampled Oct. 8, 1927. CHEATHAM COUNTY Neptune, 1% miles northeast of. Drilled well 6 inches in diameter and 165 feet deep; water from St. Louis limestone; owned by E. P. Frazier. Sam pled Oct. 10, 1927. Ashland City. Drilled well 6 inches in diameter and 69 feet deep; water from Chattanooga shale; owned by T. F. Chambliss. Sampled Oct. 10, 1927. Ashland City, 2M miles south of. Dug and drilled well 25 feet deep at former site of Sulphur Spring; water from Fort Payne formation; owned by Cheat- ham County. Sampled Oct. 10, 1927. feet deep; water from Fort Payne (?) formation; owned by E. F. Alien and others; locally known as Sunrise Spring. Sampled Oct. 10, 1927. 45 feet deep; water from St. Louis limestone; owned by Idlewild School, Petway community. Sampled Oct. 10, 1927. Kingston Spring post office, J^ mile south of. Kingston Spring; water from Fort Payne formation; owned by W. C. West. Sampled Oct. 10, 1927. water from Silurian limestone; owned by W. L. Palmore. Sampled Oct. 12, 1927. DAVIDSON COUNTY Whites Creek, 3 miles northwest of. Drilled well 6 inches in diameter and 158 feet deep; water from Fort Payne formation; owned by E. B. Hart. Sampled Sept. 14, 1927. Whites Creek, 2X miles west of. Carney's Spring; water from Chattanooga shale; owned by Mrs. George Carney. Sampled Sept. 14, 1927. 23 feet deep; water from Chattanooga shale; owned by 3. D. Carrington. Sampled Sept. 14, 1927. Ashland City, 8 miles southwest of. Young '.s Spring; water from Silurian limestone; owned by C. R. Rohrer. Sampled Sept. 13, 1927. deep; water from Leipers or Catheys formation; owned by J. C. Smith. Sampled Sept. 14, 1927. 97 feet deep; water from Catheys (?) formation; owned by Henry Farmer. Sampled Sept. 13, 1927. Nashville, 4M miles northwest of. Drilled well 6M inches in diameter and 94 feet deep; water from Hermitage formation; owned by Q. W. Bolin. Sampled Sept. 14, 1927. 1,491 feet deep; water from St. Peter (?) sandstone at depth of 1,165 feet probably mixed with water from Hermitage formation and Lebanon limestone; owned by Arthur Stevens. Sampled Sept. 14, 1927. 297 Nashville, Buena Vista Ave. "Black sulphur" spring; water from Bigby limestone; owned by Buena Vista Springs Co. Sampled Sept. 14, 1927. 298 Nashville, 1400 Eighth Ave. N. Drilled well 2,965 (?) feet deep; water probably from St. Peter (?) sandstone; owned by Morgan & Hamilton Co. Sampled Oct. 10, 1927. ° Includes iron precipitated at time of analysis. * Carbonate radicle (COs) not present. Tem pera ture C°F.) 58 61 58 58 58 58 58 58 Farrar and Foster.' 59.5 ..... do.' 60 57 61 58 58 59 60 64 62 62 66 60 68 Analyst do .... -do do .... .do. - do . .... .do . _ .do... Farrar and Foster.' Foster ...... ..... do do do . - do ... .... -do ... do- .... do do ... ..do ... Farrar and Foster.*
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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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Page 84 and 85: 68 GROUND WATER IN NORTH-CENTRAL TE
Page 88 and 89: 72, GROUND WATER IN NORTH-CENTRAL T
Page 96 and 97: 80 GROUND WATEE IN NORTH-CENTRAL TE
Page 104 and 105: TJ. S. GEOLOGICAL SURVEY WATER-SUPP
Page 110 and 111: SPEINGS 89 blank sample of water sh
Page 112 and 113: SPRINGS ' 91 formation, which are k
Page 114 and 115: SPBINGS 93 roof above its channel i
Page 116 and 117: SPKINGS bearing channel very close
Page 118 and 119: ARTESIAN CONDITIONS 97 may be expec
Page 120 and 121: 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 136 and 137: QUALITY OF GROUND WATER in north-ce
Page 138 and 139: in north-central Tennessee Continue
Page 140 and 141: QUALITY OF GROUND WATER in north-ce
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 172 and 173: Typical wells in Houston County, Te
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
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MONTGOMERY COUNTY 163 Driller's log
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MONTGOMERY COUNTY 165 and most of t
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Maximum consumption 1,200 gallons a
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e-s §8238 o o o o o o p: S JH.-C 3
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EOBEETSON COUNTY 171 GROUND-WATER C
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Typical wells in Robertson County,
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Water turbid. Stock.. .. .........
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GROUND WATEB IN NORTH-CENTRA!, TENN
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RUTHERFORD COUNTY 179 water table a
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RUTHERFORD COUNTY 181 and passing t
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RUTHERFORD COUNTY 183 tated as the
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6± miles E.. _ _ .. __ ._ _ ___ ..
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..... do... ... .... 138 ....... Ne
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58 None .............. }... .do ...
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STEWABT COUNTY 191 _ In addition to
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wash and weathered rocks in the low
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.....do....... ..... do....... Buck
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Approximate yield Openings Tempera-
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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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