GROUND WATER IN NORTH-CENTRAL TENNESSEE
GROUND WATER IN NORTH-CENTRAL TENNESSEE
GROUND WATER IN NORTH-CENTRAL TENNESSEE
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Typical springs in Wilson County, Tenn.<br />
f§ No. on<br />
-<br />
p«.<br />
Plate 4<br />
i.<br />
«4<br />
Geologic formation<br />
Approximatealtitude<br />
above sea<br />
level<br />
(feet)<br />
Topographic<br />
situation<br />
Name<br />
Owner<br />
Location with reference to nearest post office<br />
Lebanon (?) limestone.<br />
Hermitage formation.<br />
Hermitage formation or Lowville limestone.<br />
Hermitage (?) formation.<br />
Lebanon limestone.<br />
Cannon (?) limestone.<br />
Bigby (?) limestone.<br />
Lebanon (?) limestone.<br />
455<br />
570<br />
520<br />
540<br />
560<br />
725<br />
665<br />
625<br />
Valle<br />
Matt ire hill<br />
slo pe.<br />
Plain ..........<br />
Valle y ..... .<br />
Plain ..........<br />
Hills de ...<br />
Plain __ ....<br />
Undi Hating<br />
pla in.<br />
0.2. . ...<br />
Horn Spring ]S<br />
Big Spring ....<br />
311 ... .... -.<br />
Blind Fish Cave ... ....<br />
Shop Spring ...<br />
Jackson's Cave<br />
Ed. Adam<br />
J. A. Hori<br />
Roe Punu<br />
Mrs. Emn<br />
Tennessee Central Railroad,<br />
R. L. Don aid .... ... .<br />
Ed. Griffli i _ ... _<br />
Wm. Ingriham<br />
Martha, t miles N .<br />
Horn Spr<br />
Lebanon,<br />
Mount Ju<br />
Lebanon, 1H miles S"E... ... ..... .<br />
Shop Spri ng, 1^ mifcs N... ... ......<br />
Shop Spri<br />
Oladeville<br />
° 323<br />
326<br />
329<br />
»<br />
331<br />
338<br />
341<br />
342<br />
346<br />
Approximate yield<br />
Date of<br />
Gallons a measureminute<br />
ment<br />
(1927)<br />
Openings<br />
Remarks<br />
Temperature<br />
Use<br />
Variability<br />
Character<br />
Number<br />
No. on<br />
Plate 4<br />
Perennial spring.<br />
Yield by pump 3 to 5 gallons a minute; spring is site<br />
of former deer lick. Well 8 feet deep dug in orifice.<br />
Yield increases and water becomes turbid after rains<br />
to the south; noted yield is 2 days after heavy rains.<br />
Pumped 75 to 100 gallons a minute about 2 hours daily.<br />
58<br />
63<br />
Stock .............<br />
Seasonal- __ - __ ...<br />
Oct. 16<br />
150<br />
Concealed; probably beddingplane<br />
channel.<br />
1<br />
1<br />
323<br />
60<br />
Stock _ . ........<br />
Seasons<br />
Probablyseasonal<br />
.....<br />
Seasonsd.-<br />
.......<br />
a<br />
Oct. 14<br />
1,800<br />
Concealed; probably solution<br />
channel.<br />
Natural well 25 feet deep; leads<br />
to solution channel.<br />
Vertical slump and solution<br />
passage; lead to horizontal<br />
subsurface 'channel.<br />
Bedding-plane crevices.<br />
Concealed; nrobablyjoint and<br />
beddirjg-p&ne channels.<br />
Large solution channel .... ..<br />
-326<br />
320<br />
Railroad watering<br />
station.<br />
Railroad (formerly).<br />
Stock.....<br />
_ ..do .. _.<br />
None _ . .........<br />
1<br />
1<br />
Abandoned watering station.<br />
1<br />
331<br />
338<br />
Perennial spring.<br />
Do.<br />
Flows during wet season and forms intermittent creek<br />
head. Locally reported that permanent subsurface<br />
stream exists some distance within the cave.<br />
62<br />
63<br />
do<br />
do... ....... ..<br />
do. ... ........<br />
Oct. 13<br />
...do.<br />
Oct. 15<br />
10<br />
1<br />
341<br />
342<br />
None.<br />
1<br />
346<br />
gee analysis, pp. 116-J17. CO
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