GROUND WATER IN NORTH-CENTRAL TENNESSEE

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-130- Shale . use. beds found below depth of 189 feet. us -35 Near bottom. 189.... _ . Near bottom. 378 386 387 tion. above St. Louis or Warsaw limestone. tion and Cannon limestone. Ultimate capacity about 15 gallons a day. Well abandoned. water at depth of 100 feet; a third well 100 yards from No. 390 is 45 feet deep and finds fresh water at base of zone of weathering. ..... do .... ...... None ...... 40 .. 388 389 V « r v small. i Drinking .- ..... 61 -20 of Hermitage formation. Cannon or Bigby limestone. Bedding-plane crevice. Near bottom. "390 ..... do... ...... .... stone. 5+ -20... -15 .....do... .......... ...do do 391 392 bearing bed, ultimate capacity 150 gallons a day. Static level 40 feet below surface. -40 -75 90 solution channels penetrated. 62 .....do.... ............. do stone. tion. ice. .....do... ........... 393 "394 limestone. 0 1 Near bottom. None . . 60 40± . 396 397 pump. -40 -20 ice. hour. leuna with water; well abandoned. tion. limestone. stone. tion. mation. tion or Lowville limestone. 398 399 -60 ice. Limestone __ . do ... . -.do...... ... 60. ___ Near bottom. 400 401 use. -4... . -22 1-2 -25 25,60 402 403 for petroleum 870 feet deep on August 17, 1927, while drilling. Dry hole from 60 to 855 feet; sinall yield of highly mineralized water at 855 feet at top of gray magnesian (?) limestone. \'See analysis, pp. 116-117. to
218 GROUND WATER IN NORTH-CENTRAL TENNESSEE ll a ,g a ,_o Q_o ~ n - «j-j p _^ p ® fe M te § O»QO I-(CO T-4 t~ooot~ a g PQ^i. 0^ OG 00 t o o o o o SSS"5 ^ ^ ^ ^ I? ?MW ^00 ^^^ ~cL issdg
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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
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QUALITY OF GROUND WATER 101 of diss
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QUALIFY OF GROUND WATER 103 north-c
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QUALITY OF GROUND WATER 105 nesium
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QUALITY OF GROUND WATER 107 Temains
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QUALITY OF GROUND WATEB 109 undesir
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DATA waters in north-central Tennes
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QUALITY OF GROUND WATER in north-ce
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in north-central Tennessee Continue
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QUALITY OF GROUND WATER 121 more th
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5 Leipers and Cat beys formations:
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CHEATHAM COUNTY 125 which are trave
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Typical wells in Cheatham County, T
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fi7 3... .... 1± .do .... .... .
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GROUND WATEB IN NOKTH-CENTBAL TENNE
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DAVIDSON COUNTY 133 have the same w
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Typical wells in Davidson County, T
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At 1400 Eighth Ave. N. At foundry,
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Typical springs in Davidson County,
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DICKBON COUNTY 141 the Highland Rim
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DICKSON COUNTY 148 mineral matter,
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Water-bearing beds Remarks Use of w
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Typical springs in Dickson County,
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HOUSTON COUNTY 149 superficial rela
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Typical wells in Houston County, Te
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GBOUND WATEB IN NOETH-CENTEAL TENNE
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HUMPHREYS COUNTY 155 and elsewhere
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HUMPHREYS COUNTY 157 prove inadequa
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Typical wells in Humphreys County,
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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
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
Page 222 and 223: SOI hydrogen sulphide and contains
Page 224 and 225: SUMNEE COUNTY 208 Gallatin are know
Page 226 and 227: Do. hillside springs. derive water
Page 228 and 229: WILLIAMSON COUNTY Driller's log of
Page 230 and 231: WJfetlAMSON i&entf&nts, also in thf
Page 232 and 233: WILL1AMSON COUNTY 211 perennial spr
Page 234 and 235: COUNTT trated calcium bicarbonate w
Page 236 and 237: Typical wells in Williamson County,
Page 240 and 241: Approximate yield Openings Remarks
Page 242 and 243: WILSON COUNTY 221 entire Middle and
Page 244 and 245: WILSON COUNTY 223 chemical characte
Page 246 and 247: WILSON COUNTY stitute the source of
Page 248 and 249: WIIJSON COUNTY 227 associated with
Page 250 and 251: WILSON COUNTY 229 pump is driven th
Page 252 and 253: * Water-bearing beds Remarks Use of
Page 254 and 255: Typical springs in Wilson County, T
Page 256 and 257: 236 INDEX F Page Farrar, D. F., ana
Page 258 and 259: 238 INDEX Page Sumner County, munic
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GROUND WATER IN NORTH-CENTRAL TENNESSEE

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