GROUND WATER IN NORTH-CENTRAL TENNESSEE

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fi7 3... .... 1± .do .... .... . »265 the vicinity from dug wells about 25 feet deep. 58 do.... ... -25 ... -40 stone. tion. stone. formation. torn. 70 144. _ .... 267 »269 drilled. from well in development; ultimate capacity about 1 gallon a minute 1±~ -125- ice. filled by silt. Vffi 1 See analysis, pp. 114-115. Typical springs in Cheatham County, Tenn. Geologic formation Approximatealtitude above sea level (feet) Topographic situation Name Owner Location with reference to nearest post office No. on Plate 4 Hillside Valley Plateau Valley.. __ do... ...... dO Hillside . Valley Hillside Valley do H. O. Knox- __ . ......... 3. W. Cage & Co.- __ ..... Thomasville, 2 miles NE ________ Do. Do. Do. Do. Mill Spring. Tom Nichols.. .............. Chapmansboro, Smiles NE ............. Ashland City, 4 miles N Ashland City, % miles NE. ___ . _ . Do. Do. Do. 595 550 660 500 460 605 435 625 425± 396 535 510 W. C. West. _________ Kingston Springs, Ji mile S _______ 239 241 242 246 247 249 260 262 256 259 266 268 [Table continued on p. 130]
Typical springs in Cheatham County, Tenn, Continued 00 o Approximate yield Openings Remarks Temperature (°F.) Use Variability Date of measurement (1927) No. on Plate 4 Gallons a minute Character Number Natural well leading to underground channel. Yield increases and water becomes turbid about 12 hours after rain to the south. Perennial spring. Roadside spring and watering trough. Turbid after several days' continuous rain. Emergency supply for Ashland city. Reported minimum discharge 100 gallons a minute. Aug. 21 1 1 239 241 59 58 59 58 Drinking, stock ... ... ..do.... .... .....do ......... ..... Aug. 20 Aug. 21 Aug. 20 25 20 1-2 100 .....do .... .do... .... .do ................. ..... 1 242 245 247 58 59 57 58 Domestic, stock ... Domestic, stock _ .... .do ....... ... Probably seasonal .....do ....... ....... ... ..do .............. do ...do.... do . Aug. 22 50 1± 10 5± . .do... Perennial spring. Do. 1 Many. 1 2 249 250 252 256 Used locally as medicinal water. Discharge may percolate through creek gravel in large part. Medicinal sulphur spring. So-called freestone spring near by has its source in weathered zone of rock. 59 57 Aug. 22 do . No flow. 5-8 1A± Joint and bedding-plane channels. Slumped roof of underground channel. 61 259 266 268 1 See analysis, pp. 114-115.
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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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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 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 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 196 and 197: Water turbid. Stock.. .. .........
Page 198 and 199: 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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