GROUND WATER IN NORTH-CENTRAL TENNESSEE
GROUND WATER IN NORTH-CENTRAL TENNESSEE
GROUND WATER IN NORTH-CENTRAL TENNESSEE
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8<br />
Typical wells in Davidson County, Tenn. Continued<br />
[All drilled wells]<br />
Water-bearing beds<br />
Remarks<br />
Use of water<br />
Temperature<br />
(°F.)<br />
Yield<br />
(gallons<br />
a minute)<br />
Method of lift<br />
Water<br />
level<br />
above<br />
or<br />
below<br />
surface<br />
(feet)<br />
Depth below<br />
surface<br />
(feet)<br />
No. on<br />
Plato 4<br />
Geologic horizon<br />
Character of<br />
material<br />
Automatic electric<br />
pump.<br />
TopofFortPayne<br />
formation.<br />
Catheys (?) formation.<br />
Bigby (?) limestone.<br />
Fort Payne formation.<br />
Chattanooga shale<br />
Silurian limestone-<br />
..... do... ... ... ....<br />
Leipers (?) formation.<br />
Bigby (?) limestone.<br />
Leipers or Catheys<br />
formation.<br />
Hermitage (?) formation.<br />
-do .....<br />
Lowville (?) limestone.<br />
Hermitage (?) formation.<br />
Catheys (?) formation.<br />
Leipers formation.<br />
Hermitage formation.<br />
St. Peter (?) sandstone.<br />
76.. ....<br />
Public well at Amqui station. Reported to<br />
flow in wet seasons.<br />
One of several wells at abandoned explosives<br />
plant.<br />
Supply ample in extreme drought.<br />
60<br />
12±<br />
3-5..<br />
-40 ...<br />
-15<br />
Near bottom.<br />
185........<br />
155± ...<br />
20.........<br />
30.........<br />
272<br />
275<br />
-125..<br />
do ... ... .....<br />
Cherty limestone ..<br />
Shale .<br />
do . .... ...<br />
Cherty limestone ...<br />
Shale... . .<br />
~do<br />
Bedding-plane crevice.<br />
276<br />
«277<br />
58<br />
59<br />
Well at new residence on east side of Eaton<br />
Creek.<br />
Water too hard for laundering.<br />
In Gordonia community.<br />
.. do ...... ....<br />
..... do .... ...<br />
Stock.. . -<br />
Domestic, stock ...<br />
.... . do .......<br />
3-5<br />
H ...<br />
"16"<br />
5- _<br />
3-5. _ .<br />
Gasoline force pump..<br />
-6<br />
-20<br />
-40<br />
-15 ...<br />
a 279<br />
280<br />
281<br />
284<br />
40±. ......<br />
90.........<br />
285<br />
Reported tested at 18 gallons a minute without<br />
notable drawdown.<br />
64<br />
5± -<br />
8. ......<br />
..do ..............<br />
2± -<br />
-30<br />
-50<br />
59.........<br />
160.. ...<br />
286<br />
287<br />
..... do. ...<br />
.do .... ...<br />
Well abandoned because of pollution by oil<br />
waste from near-by garage.<br />
Ample for 3 families in extreme drought.<br />
-50<br />
-35<br />
100± ...<br />
92.........<br />
289<br />
290<br />
60<br />
62<br />
58<br />
62<br />
66<br />
3<br />
-20<br />
.....do -<br />
Bedding-plane crevice.<br />
Near bottom.<br />
..do..<br />
291<br />
292<br />
Ultimate capacity about 2 gallons a minute.<br />
Stock-. .<br />
..... do ... ..... ..<br />
-60<br />
+3H--<br />
... -do ....<br />
Sandy limestone. . .<br />
90....<br />
1,165......<br />
293<br />
294<br />
Fresh water at 85 feet hi Hermitage formation;<br />
sulphur water at 195 feet in Lebanon (?) limestone.<br />
Casing pulled and water probably<br />
from several beds.<br />
35<br />
295<br />
Garden irrigation _<br />
20<br />
-45<br />
Hermitage formation.<br />
Solution crevice-<br />
100<br />
296
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