GROUND WATER IN NORTH-CENTRAL TENNESSEE
GROUND WATER IN NORTH-CENTRAL TENNESSEE
GROUND WATER IN NORTH-CENTRAL TENNESSEE
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At 1400 Eighth Ave. N.<br />
At foundry, 217 Third Ave. N. Maximum consumption<br />
10,000 gallons a day. A second<br />
well near by is 500 feet deep.<br />
At 607 Tenth Ave. N. Three wells drilled and<br />
sprung with 200 sticks dynamite each to open<br />
Drinking, foundry<br />
68<br />
62<br />
5 .<br />
15<br />
Artesian flow and air<br />
lift.<br />
+75 (?)<br />
+8....<br />
St. Peter (?) sandstone,<br />
-...do ....... ..<br />
1, 100 (?)<br />
'298<br />
299<br />
Bigby limestone or<br />
Hermitage formation.<br />
Lebanon (?) lime-1<br />
stone. 1<br />
Eidley (?) lime-[<br />
stone. j<br />
St. Peter (?) sandstone.<br />
300<br />
crevices to buried spring.<br />
/At 916 Fourth Ave. N. Maximum capacity of<br />
\ well tested at 228 gallons a minute.<br />
At Fourth Ave. and Church St. Ultimate<br />
capacity tested at 100 gallons an hour and<br />
well abandoned.<br />
Dry hole in divide between meanders of Cumberland<br />
River.<br />
Well at Newsom section houses. Capacity<br />
tested by bailer at 20 gallons a minute; waterbearing<br />
crevices of small yield at depth of 60<br />
and 95 feet.<br />
63<br />
228<br />
>Deep-well turbine.- ...<br />
-28<br />
-60<br />
(Solution channels<br />
I filled with sand.<br />
J128<br />
1289 .....<br />
1,100±_._.<br />
-302<br />
None --------<br />
L es S-<br />
than2<br />
+Slight<br />
303<br />
..do<br />
......<br />
3-5<br />
Hand pump .. ..<br />
-60<br />
Leipers formation.<br />
195. ....<br />
307<br />
309<br />
Public well at Newsom station.<br />
Public well at Belleview station.<br />
No water-bearing beds below 103 feet.<br />
Well at Vaughns Gap section houses; supplies<br />
9 families.<br />
No water-bearing beds below 98 feet.<br />
Water contains oily material in emulsion.<br />
Other wells in this vicinity which reach same<br />
horizon yield M to 2 gallons a minute.<br />
Five test wells each yielded enough for a household<br />
supply; inadequate for hospital needs.<br />
Water-bearing channel at same altitude as bed<br />
of Stone River.<br />
Dry hole; bottom in Hermitage formation. ±<br />
3.<br />
3-5<br />
..... do...<br />
-45<br />
-10<br />
60<br />
60<br />
.....do.. .....<br />
Catheys formation.<br />
Bigby (?) limestone.<br />
Leipers (?) formation.<br />
Bigby (?) limestone.<br />
Hermitage (?) formation.<br />
Lowville (?) limestone.<br />
Catheys (?) formation.<br />
..... do. .<br />
do.<br />
90<br />
52. .<br />
136 ....<br />
310<br />
311<br />
312<br />
Bedding-plane crevice.<br />
5 ....<br />
3<br />
H<br />
Automatic electric<br />
pump.<br />
-101-<br />
-136-<br />
Small solution crevice.<br />
60<br />
101........<br />
200. ....<br />
do .....<br />
... ..do ......<br />
do .. __ .<br />
08<br />
313<br />
314<br />
315<br />
58<br />
60<br />
3_ .<br />
3. .<br />
do .<br />
-...do ...... ... ..<br />
..... do .......<br />
Near bottom.<br />
50 .<br />
«316<br />
317<br />
58<br />
-100-<br />
Lebanon (?) limestone.<br />
Hermitage formation.<br />
Lebanon limestone.<br />
Bedding-plane crevice.<br />
100 . _ .<br />
318<br />
319<br />
None. __ ___ ..<br />
None.<br />
2<br />
-85<br />
-60<br />
Shale<br />
..... do....... .... ...<br />
120. ....<br />
90....<br />
320<br />
321<br />
..... do... ....... ...<br />
322<br />
See analysis, pp. 114-117.<br />
CO
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