GROUND WATER IN NORTH-CENTRAL TENNESSEE
GROUND WATER IN NORTH-CENTRAL TENNESSEE
GROUND WATER IN NORTH-CENTRAL TENNESSEE
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36 <strong>GROUND</strong> <strong>WATER</strong> <strong>IN</strong> <strong>NORTH</strong>-<strong>CENTRAL</strong> <strong>TENNESSEE</strong><br />
part of the formation consists of beds of somewhat earthy blue lime<br />
stone between 2 and 18 inches thick, which are accompanied by quartz<br />
geodes from 1 to 12 inches in diameter and by nodular and irregular<br />
tabular masses of chert. The amount of chert decreases noticeably<br />
and the proportion of earthy limestone and calcareous shale increases<br />
from the top of the formation toward the bottom. In the south-<br />
central and southwestern parts of the region, especially in Williamson,<br />
Dickson, and Humphreys Counties, the upper part of the formation<br />
includes many beds of coarse sandy limestone or calcareous sandstone,<br />
whose weathered and leached outcrops resemble buff sandstone.<br />
Locally, in the same district, the lower part of the formation, according<br />
to Safford,52 is a massive blue-gray limestone whose maximum thick<br />
ness is 150 feet. According to Mather & the upper 50 to 60 feet of the<br />
formation in the northeastern part of the region, in Simmer County,<br />
consists of thin-bedded buff or brownish-gray limestone that contains<br />
numerous geodes and much tabular chert. This upper division is<br />
underlain by about 30 feet of relatively pure coarsely crystalline lime<br />
stone hi massive beds, which inclose tabular masses of light-brown or<br />
milky-white chert from 3 to 12 inches thick that become less abun<br />
dant in the lower beds of the division. Estimates by several geologists<br />
of the thickness of the Fort Payne formation range from 90 to 275 feet,<br />
although the stratigraphic limits of the sections covered by these<br />
estimates, especially the lower limit, may not be strictly equivalent.<br />
The Fort Payne formation is essentially nonfossiliferous in north-<br />
central Tennessee, although locally, as in western Overton County,64<br />
the upper 20 feet contains many fragments of crinoids, the presence of<br />
which differentiates these beds from the overlying Warsaw formation.<br />
However, fossils are comparatively abundant in the Fort Payne of<br />
other areas and also in beds that underlie the Fort Payne. The for<br />
mation is now classified by Butts,55 who has studied the formation over<br />
a broad region in Kentucky, Tennessee, and Alabama, as containing<br />
beds of Keokuk, Burlington, Fern Glen, and late Kinderhook age.<br />
The Fort Payne formation forms the Highland Rim plateau in<br />
eastern Sumner County and crops out extensively over the middle and<br />
lower slopes of the dissected part of the plateau along the Highland<br />
Rim escarpment and in the valleys of the Tennessee and Cumberland<br />
Rivers. The formation is deeply weathered throughout the upland<br />
areas, and the weathering has generally produced a reddish or<br />
yellowish-buff soil that contains much dense chert in subangular<br />
fragments. In many places the tabular chert has not disintegrated,<br />
although the calcareous matter of the intervening limestone layers<br />
« Safford, J. M., Geology of Tennessee, p. 340,1869.<br />
» Mather, K. F., op. cit., p. 24.<br />
s* Butts, Charles, op. cit., p. 15.<br />
« Butts, Charles, Geology of Alabama: Alabama Geol. Survey Special Kept. 14, pp. 166-167,1926.