GROUND WATER IN NORTH-CENTRAL TENNESSEE

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DATA waters in north-central Tennessee and D. F. Farrar, Tennessee Geological Survey, analysts] Total dis solved solids at 180° C. 50 132 198 196 220 143 71 262 148 2,970 1,948 336 174 1,238 318
112 GROUND WATER IN NORTH-CENTRAL TENNESSEE Jfo. on Tlate4 115 120 IB 121 F" 126 127 .131 132 135 137 138 143 149 151 159 161 164 167 171 173 177 180 190 191 198-A Location and description SUMNER COUNTY Analyses of representative ground waters limestone; owned by John Baskerville; municipal supply of Portland. Sampled Oct. 19, 1927. Westmorland, 5 miles west of. Oil test well 5^i inches in diameter and 100 feet deep; water from bed just above or below Chattanooga shale; owned by R. O. Troutt. Sampled Oct. 19, 1927. deep; water from chert residuum above Fort Payne formation; owned by Sumner County High School. Sampled Oct. 18, 1927. White House, 2M miles south of. Tyree Spring; water from weathered zone of Fort Payne formation; owned by Mrs. Cartwrigbt. Sampled Oct. 20, 1927. mation; owned by O. W. Mitchell. Sampled Oct. 20, 1927. Saundersville, 2}i miles northwest of. Drilled well 20 feet deep; water from shaly facies of Leipers (?) formation; owned by John Mirs. Sampled Oct. 20, 1927. owned by J. R. Durham. Sampled Oct. 20, 1927. Qallatin. Drilled well 8 inches in diameter and 300 feet deep; water from Bigby (?) limestone at approximate depth of 200 feet; owned by Louisville & Nashville R. R. Sampled Oct. 18, 1927. Castalian Springs post office. Castalian Spring; water from Bigby lime stone or upper part of Hermitage formation; owned by Q. W. Wynne. Sampled Oct. 18, 1927. HOUSTON COUNTY stone; owned by Largent Bros. Sampled Oct. 6, 1927. Erin, 0.6 mile west of. Unnamed spring from St. Louis limestone; owned by A. J. Mitchum; municipal supply of Erin. Sampled Oct. 6, 1927. deep; water from Fort Payne formation; owned by Steve Batson. Sam pled Oct. 6, 1927. deep; water from Fort Payne (?) formation; owned by Yellow Creek High School. Sampled Oct. 7, 1927. HUMPHREYS COUNTY owned by Milton Petty. Sampled Oct. 6, 1927. gravel; owned by Luther Haygood. Sampled Oct. 7, 1927. McEwen, 14 mile northeast of. Drilled well 8 inches in diameter and 217 feet deep; water from chert residuum above St. Louis or Warsaw limestone at depth of 80 feet; owned by McEwen School. Sampled Oct. 7, 1927. deep; water from weathered St. Louis of Warsaw limestone; owned by Nashville, Chattanooga & St. Louis Ry., municipal supply for Waverly. Sampled Oct. 6, 1927. deep; water from chert residuum above Fort Payne formation; owned by J. M. C. Young. Sampled Oct. 7, 1927. owned by L. L. Shipp. Sampled Oct. 7, 1927. Bold Springs post office. Bold Spring; water from St. Louis (?) limestone; owned by J. R. James. Sampled Oct. 6, 1927. Denver, 4J4 miles south of. Sulphur Spring; water from Silurian (?) lime stone; owned by D. M. McCrary. Sampled Oct. 7, 1927. DICKSON COUNTY Stayton, 2% miles north of. Drilled well 5 inches in diameter and 65 feet deep; water from Fort Payne formation; owned by John Freeman. Sampled Oct. 8, 1927. Stayton, 3 miles north of. Drilled well 6 inches in diameter and about 40 feet deep; water from Fort Payne formation; J. L. Tilley, renter. Sampled Oct. 8, 1927. Vanleer, 5 miles west of. Drilled well 5^i inches in diameter and 65 feet deep ; water from Fort 'Payne formation (?) ; W. R. Berry, owner. Sampled Oct. Tem pera ture C°F.) 58 56.5 57 58 58 62 EC 53 60 Kfi 57 57 58 56 ' ......do..... 58 5$ 61 57 5$ 57 60 56 58 59 k Analyst Foster.. _ Farrar and Foster.* Farrar and Foster.' do~ Farrar and Foster.' do.. .do - .... .do. . do- do do-. Farrar Farrar and Foster.* .do.' «Includes iron precipitated at time of analysis. * Carbonate radicle (COj) not present. «Calculated
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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 82 and 83: 66 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 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
Page 180 and 181: 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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