GROUND WATER IN NORTH-CENTRAL TENNESSEE

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QUALITY OF GROUND WATEB 109 undesirable bacteria by periodic sanitary analyses. All ground water that issues from channeled limestone, .if used as municipal supply, should preferably be sterilized by a suitable chlorinating apparatus as a routine precaution against pollution. Under most conditions such sterilization does not impart taste or odor to the water if the operation is properly controlled.
110 GROUND WATER IN NORTH-CENTRAL TENNESSEE No. on Plate 4 1 6 19 24 27 32 35 42 AA. TTt 54 57 64 67 68 71 Location and description STEWABT COUNTY ANALYTICAL Analyses of representative ground ; [Margaret D. Foster, IT. S. Geological Survey, Model, 5}4 miles west of. Cedar Spring, water from Fort Payne formation; owned by W. C. Outland. Sampled Oct. 5, 1927. Bumpus Mills, % mile south of. Drilled well 6 inches in diameter and 48 feet deep; water from chert residuum above St. Louis or Warsaw limestone; owned by W. P. Luten. Sampled Oct. 5, 1927. Dover, 5% miles northwest of. Drilled well 6 inches in diameter and 75 feet deep; water from gravel (weathered chert nodules) ; owned by B . F. Riggins. Sampled Oct. 5, 1927. Indian Mound, 4}^ miles north of. Drilled well 5$l inches in diameter and 164 feet deep; water from St. Louis or Warsaw limestone; owned by estate of Mrs. Bert Smith. Sampled Oct. 4, 1927. Indian Mound. Drilled well 55 feet deep; water from St. Louis or Warsaw limestone; owned by C. K. Keatts. Sampled Oct. 4, 1927. Mobley, 3M miles northwest of. Wofford Spring; water from Fort Payne formation; owned by J. W. Wofford. Sampled Oct. 5, 1927. Mobley, 4^4 miles east of. Unnamed spring from Fort Payne formation; owned by estate of W. H. Cox. Sampled Oct. 5, 1927. MONTGOMEEY COUNTY Woodlawn, 5 miles northwest of. Drilled well 551 inches in diameter and 136 feet deep; water from St. Louis or Warsaw limestone; owned by E. B. Ingraham. Sampled Oct. 4, 1927. Woodlawn, 5}4 miles northeast of. Britton Spring; water from St. Louis or Warsaw limestone; owned by H. E. Killebrew. Sampled Oct. 4, 1927. St. Bethlehem, 2J£ miles southwest of. Idaho Spring; water from alluvium overlying St. Louis or Warsaw limestone; owned by J. H. Unseld. Sampled Oct. 4, 1927. Clarksville, 4}^ miles east of. Drilled well 6 inches in diameter and 162 feet deep; water from St. Louis or Warsaw limestone, leased by W. R. Corlew. Sampled Oct. 4. 1927. Hackberry. Drilled well 6 inches in diameter and 50 feet deep; water from St. Louis or Warsaw limestone; owned by Henry Yarber and James Broom. Sampled Oct. 4, 1927. Louise, 4 miles southwest of. Unnamed spring from St. Louis or Warsaw limestone; owned by George W. Bryant. Sampled Oct. 4, 1927. Louise, 5 miles southeast of. Drilled well 5 inches in diameter and 65 feet deep; water from Fort Payne formation; owned by C. D. Batson. Sampled Oct. 4, 1927. Hickory Point, 6M miles northeast of. Dug well 4 fdet in diameter and about 60 feet deep; water from chert residuum above St. Louis or Warsaw limestone; owned by George Watson. Sampled Oct. 4, 1927. EOBEETSON COUNTY 73 Adams, S^4 miles northwest of. Mint Spring; in basal St. Louis limestone; owned by Joel Fort. Sampled Oct. 9, 1927. 81 Springfield, 10 miles north of. Drilled well 5
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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 80 and 81: 64 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 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 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
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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
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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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