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GROUND WATER IN NORTH-CENTRAL TENNESSEE

GROUND WATER IN NORTH-CENTRAL TENNESSEE

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STRATIGRAPHY 25<br />

In general the occurrence of ground water in any region depends<br />

in some measure upon the texture of the rocks, so that the stratig­<br />

raphy is a guide to the development of ground-water supplies. Hence<br />

the stratigraphy of north-central Tennessee is here discussed in some<br />

detail. However, few of the stratigraphic units have a distinctive<br />

lithology over any large portion of the area, so that identification of<br />

the beds must rest upon the contained fossils, and it is difficult to<br />

apply in practice the relations between stratigraphy and occurrence<br />

of ground water.<br />

The stratigraphic sequence and general lithologic character of the<br />

rocks are summarized in the following table, and each of the strati-<br />

graphic units is described in the succeeding pages. The sequence of<br />

description, however, is the inverse of that which is usually followed<br />

in geologic reports, in that the formations are described from the top<br />

of the geologic column downward that is, in the order in which they<br />

are encountered by the driller.<br />

100144 32 3

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