GROUND WATER IN NORTH-CENTRAL TENNESSEE

More documents

Recommendations

Info

5 Leipers and Cat beys formations: Waters containing less than 1,000 parts per million dissolved solids (analyses 127, 131, 132, 286, 317) Average ... OQ 71 163 .67 .12 1.4 14 9 0 20 Minimum ___ . . __ . . *5.5 364 253 481 437 292 628 .35 .05 .6 20 2.9 48 114 49 198 282 237 364 1Q 5.0 26 26 16 43 Waters containing more than 1,000 parts per million dissolved solids (analyses 292, 311, 394
124 GROUND WATER IN NORTH-CENTRAL TENNESSEE In general, the ground water associated with the Chattanooga shale near its outcrop is "black sulphur" water, iron being taken into solution as the sulphate from oxidized portions of the pyritiferous shale and the sulphate being reduced by the carbonaceous matter of the shale. Generally the water contains less than 500 parts per million of dissolved mineral matter and the hydrogen sulphide is less than 10 parts per million. The water associated with the crystalline Silurian limestones has the least average content of dissolved solids, is relatively soft, and has little noncarbonate hardness; hence it is suitable for many uses without any preliminary treatment. The water that issues from the Bigby limestone generally contains more matter in solution and appreciably more sodium and potassium than the water carried at similar depth by other stratigraphic units of the same water-yielding capacity. At several localities, especially in the vicinity of Nashville, the dense limestone beds of the Cannon and Bigby limestones contain blebs of petroliferous material, and some of the associated ground water contains sufficient oil in the emulsified state to impart a disagreeable taste and a pronounced opalescence. Other than these general relations, however, little correlation can be made between chemical character of the ground water and the stratigraphic horizon of the water-bearing bed. SUMMARY DESCRIPTIONS BY COUNTIES CHEATBAM COUNTY [Area, 314 square miles. Population, 9,025 ] GENERAL FEATURES Cheatham County lies in the geographic center of the area covered by this report and is bounded on the north by Montgomery and Rob- ertson Counties, on the east by Davidson County, on the south by Williamson County, and on the west by Dickson County. The area is wholly rural. The county seat and largest community, Ashland City (population, 712) is situated in the valley of the Cumberland River on the Tennessee Central Railroad. Cheatham County includes the stream gaps by which the Nashville Basin drains northwestward across the Highland Rim Plateau (see pp. 16-18) and hence has a rather rugged topography. From the Cum berland River northward the surface is a dissected plateau comprising flat and gently rolling interstream tracts whose altitude ranges from 700 to 780 feet above sea level and closely spaced subparallel youthful drains adjusted to the Cumberland River at 350 feet above sea level. Sink-hole topography exists locally on these interstream plateau tracts but is not characteristic of them within Cheatham County. The topography of the central and southern parts of the county, '» Figures for population from 1930 census.
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 42 and 43:
Stratigraphic section for north-cen
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 50 and 51:
Page 52 and 53:
Page 54 and 55:
TJ. S. GEOLOGICAL SURVEY WATER-SUPP
Page 56 and 57:
XT. S. GEOLOGICAL SUKVEY WATER-SUPP
Page 58 and 59:
Page 60 and 61:
Page 62 and 63:
Page 64 and 65:
Page 66 and 67:
Page 68 and 69:
52 GEOTJND WATBE IN NOETH-CBNTEAL T
Page 70 and 71:
Page 72 and 73:
Page 74 and 75:
j GEOUND WATEE IN NOETH-CENTEAL TEN
Page 76 and 77:
Page 78 and 79:
Page 80 and 81:
Page 82 and 83:
Page 84 and 85:
Page 86 and 87:
Page 88 and 89:
72, GROUND WATER IN NORTH-CENTRAL T
Page 90 and 91:
Page 92 and 93:
Page 94 and 95: 78 GROUND WATER IN NORTH-CENTRAL TE
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 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 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 196 and 197:
Water turbid. Stock.. .. .........
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
Page 246 and 247:
WILSON COUNTY stitute the source of
Page 248 and 249:
WIIJSON COUNTY 227 associated with
Page 250 and 251:
WILSON COUNTY 229 pump is driven th
Page 252 and 253:
* Water-bearing beds Remarks Use of
Page 254 and 255:
Typical springs in Wilson County, T
Page 256 and 257:
236 INDEX F Page Farrar, D. F., ana
Page 258 and 259:
238 INDEX Page Sumner County, munic
show all

GROUND WATER IN NORTH-CENTRAL TENNESSEE

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?