GROUND WATER IN NORTH-CENTRAL TENNESSEE

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Stratigraphic section for north-central Tennessee Continued to 00 Water-bearing properties Character of strata Thickness (feet) Formation Correlation Series System Soft green or chocolate-colored shale with bands of coarsely crystalline gray and mottled phosphatic limestone. Blue granular crystalline limestone with interbedded shale. Knotty earthy limestone and interbedded shale, or granular crystalline limestone without shale. Knotty earthy limestone and shale with heavy bands of impure blue limestone. Massive pure dove-colored and gray limestone, also earthy cherty blue limestone. Mainly granular crystalline gray or brown laminated and cross-bedded phosphatic limestone. At western edge of Nashville Basin chiefly medium-bedded sandy and phosphatic subgranular limestone with local beds of shale. Toward the northeast and east grades into Saggy bluegray sandy and earthy limestone, calcareous sandstone, and shale. Upper member consists of thin-bedded dovecolored limestone and yellowish-gray shale. Lower member (Carters limestone restricted) is massive compact white or light-blue cherty limestone. 0-40 Fernvale formation. Richmond Upper Or- 0-3 Arnheim limestone. 0-100 Leipers limestone. Maysville group. 50-100 Catheys limestone. 0-250 Cannon limestone. 30-100 Bigby limestone. Trenton group. Middle Ordovician. 40-80 Hermitage formation. Water-bearing properties of the pre-Mississip- place and are dependent upon (1) solubility of the rock; (2) intensity of jointing, which is in turn dependent upon (a) competency of the stratum, (6) localization of stresses; (3) geomcrphologic history of the district. Lower part of Black River group. Ordovician. 40-110 Lowville limestone.
Thin-bedded compact bluish-gray, dove-colored, or brown limestone with parangs of yellow clay; beds 1 to 6 inches thick; fossils abundant at many localities. Massive fine-grained blue-gray to brown cherty limestone; not highly fossiliferous. Thin-bedded blue or drab brittle limestone with local heavy beds of bluish-brown coarse crystalline limestone; highly fossiliferous. Massive brittle drab cherty limestone. 80-125 Lebanon limestone. 95-120 Eidley limestone. I h 1 tf Chazy group Lower Ordovidan. 23-28 Pierce limestone. Murfreesboro limestone. -Unconformity J02 70+ Light-gray fine-grained, slightly cherty magnesian limestone of the Wells Creek Basin, Stewart County. Beekmantown group K> SO
Page 1 and 2: PLEASE DO NOT DESTROY OB THROW AWAY
Page 3 and 4: CONTENTS Pager -Abstract.__________
Page 5 and 6: OOHTBHTS V Ground water Continued.
Page 7 and 8: ABSTRACT This report describes brie
Page 9 and 10: GBOUND WATEB IN NOBTH-CENTBAL TENNE
Page 11 and 12: INTBODUCTION Q In addition to the w
Page 13 and 14: GEOGRAPHY O exist at several locali
Page 15 and 16: GEOGRAPHY / The annual range betwee
Page 17 and 18: J? §1 ? 20 158 2 20 15 GEOGRAPHY 9
Page 19 and 20: Record lacking for 1882, 1887-88, 1
Page 21 and 22: GEOGRAPHY 13 In general there is so
Page 23 and 24: SURFACE FEATURES OF CENTRAL TENNESS
Page 25 and 26: StJBFACE FEATURES OF CENTRAL TENNES
Page 27 and 28: SURFACE FEATURES OF CENTRAL TENNESS
Page 29 and 30: STJBFACE FEATURES OF CENTRAL TENNES
Page 31 and 32: SURFACE FEATUKES OF CENTKAL TENNESS
Page 33 and 34: U. S. GEOLOGICAL SUBVEY WATEH-STJPP
Page 35 and 36: U. 8. GEOLOGICAL STJEVEY WATER-SUPP
Page 37: U. S. GEOLOGICAL SURVEY WATER-SUPPL
Page 40 and 41: to O> Stratigraphic section for nor
Page 44 and 45: 30 GROUND WATER IN NORTH-CENTRAL TE
Page 46 and 47: 32 GEOTJND WATEE IN NOETH-CENTEAL T
Page 48 and 49: 34 GEOTJND WATER IN NORTH-CENTRAL T
Page 54 and 55: TJ. S. GEOLOGICAL SURVEY WATER-SUPP
Page 56 and 57: XT. S. GEOLOGICAL SUKVEY WATER-SUPP
Page 68 and 69: 52 GEOTJND WATBE IN NOETH-CBNTEAL T
Page 74 and 75: j GEOUND WATEE IN NOETH-CENTEAL TEN
Page 88 and 89: 72, GROUND WATER IN NORTH-CENTRAL T
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76 GROUND WATER IN NORTH-CENTRAL TE
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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
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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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