GROUND WATER IN NORTH-CENTRAL TENNESSEE

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Water turbid. Stock.. .. ......... 101 saw limestone 0). torn. -60... .....do.. .......... of less than 100 feet had very small yield. 67 5±._... 5± . 1-2 __ pump. .. _ do. _ ... ... Hand pump ......_... -52... crevice. ..... do. .do ........ .... .do ... ..... ..... do. ..... ... do_ ... do 115 . 102 103 104 irys saw limestone. saw limestone (Tfc Stock. . Small 64 +1... ..... do.... ... ... ... torn. ...do ... 125 ____ 107 ins bottom; top of Chattanooga shale at 165 feet. No water-bearing beds below 166 feet. mation. 68 35 -79... matioa. mation. tion. formation. crevice. ..... do.. ........ .. 3-5. . 3-5.. torn. QfiJ- 5fi .. do.... ... .. 109 110 112 -150- 155 113 Louisville & Nashville R. R. tunnel was driven at Eidgetop. Drainage by tunnel has lowered ground-water level 75 feet in vicinity. See analysis, p. 110-111.
Typical springs in Robertson County, Tenn. Geologic formation Topographic situation Name Owner Location witb reference to nearest post office No. on Plate 4 St. Louis limestone. St. Louis or Warsaw limestone. Do. Do. Do. Do. Do. Do. Do. Fort Payne (?) formation. Fort Payne formation. Approximate altitude above sea level (feet) 400 575 495 700 605 655 575 590 630 700 780 Valle y dn . . do ___ _ .. Plate Valle y.. Hills dn d" VaUe Plate do Mill Cave .. .._ Ig ...... Mclntosh Sprii lg Perry's Park S Worsham Sprii 'Ffygpjft Spring Joel Fort John Snee< 1.. ....... ...... .. W. M. Qo> City of Or! J. W. Dral James Pay Will Powe 11 Arthur Po J H PernJr . _ R. B. Beal . .............. Adams, 3} Cedar HiJ 1, 3M miles NE. . QedarHil 1, 4% miles NE-.... ......... Qrlinda, 1 mile SB. __ . ________ . Orlinda, 1 H miles S_ _. .............. Orlinda, 6 Springfleh i, 3 miles W......... _.. .. Sprmgfiel( I, 2M mUes N. . ........ Springfielc 1, 1 mile S....... ........ ........ Springfielc 1, 5 miles SE _ ---.__. _ .-_ Greeobrie r, \\i miles SE . , 73 79 80 89 90 91 96 97 100 105 111 Approximate yield Date Of Gallons a measureminute ment (1927) Openings Remarks Temperature (°F.) Use Variability Cbaracter Number No. on Plate 4 Flow increases and water becomes turbid after protracted rain. Yield noted is total from 5 openings in a zone 200 yards long. Yield noted 150 yards below spring outlet. In wall of sink hole on Highland Him plateau. Flow increases and water Becomes turbid 3 hours or 58 59 59 60 57 Season, ai.. ............ .....do . .do do do........ .... ..... Aug. 26 ...do .. 100 25 725 10± 50=fc f . 30 I 50 r 75 t 175 "H 1 5 73 Domestic, stock _ Stock ______ . do..... ................. ... ...do... .. Aug. 27 _ do .. Small bedding-plane channel.. 1 79 80 89 90 more after heavy rain. Flow increases and water becomes turbid after long rain. Do. 57 58 58 }. ,do .... }... .do.... ...... ...do Oct. 8 Aug. 24 Oct. 9 Aug. 4 Aug. 25 . __ do. _______ .- _ . Bedding-plane solution channel. 1 1 1 1 1 a 91 «96 Domestic, stock... do ...... Formerly had considerable yield. Spring failed after heavy blasting in near-by quarry. 97 100 105 64 63 Medicinal formerly. Season,al (?) .. Aug. 25 Trickle.... 111 1 See analysis, pp. 110-111.
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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:
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
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 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 238 and 239: -130- Shale . use. beds found below
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
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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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