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GROUND WATER IN NORTH-CENTRAL TENNESSEE

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42 <strong>GROUND</strong> <strong>WATER</strong> <strong>IN</strong> <strong>NORTH</strong>-<strong>CENTRAL</strong> <strong>TENNESSEE</strong><br />

similar in lithology to the rock of the type section and is characterized<br />

by species of Heliophyttum, Blothrophyttum, Oystiphyttum, Cyathophyl-<br />

lum, Cladopora, and Bryozoa. Foerste 77 correlated the upper part of<br />

the formation with the Sellersburg limestone of Indiana, which is of<br />

late Middle Devonian (Hamilton) age, and implied that the lower<br />

part was of early Middle Devonian ("Comiferous" Onondaga) age.<br />

Dunbar 78 has correlated the entire formation with the Jeffersonville<br />

limestone of Indiana, which is early Middle Devonian (Onondaga).<br />

The Pegram limestone is undoubtedly separated from the under­<br />

lying strata by a disconformity at the two localities that have been<br />

described.<br />

Recently Pohl 79 has shown that limestone of upper Pegram age is<br />

accompanied locally by an underlying sandstone member, of probable<br />

lower Pegram age, whose maximum known thickness is 35 feet. He<br />

describes the type section and occurrence of this member as follows:<br />

Section in district 4, Trousdale County, Term., in road cut on hill 1% to 1% miles<br />

southwest of Valentine's store<br />

Mississippian:<br />

Chattanooga shale Feet<br />

Dead-black, thinly fissile shale with thin bed of conodont-bearing<br />

sandstone at base__.___ To top of hill.<br />

Gray blocky shale carrying abundant Lingulas and<br />

a few Mississippian conodonts________________ 7<br />

Possible break.<br />

Devonian (?): Black shale like first with lenses of fine, black<br />

sandstone near base, grading without apparent break<br />

into limestone below--______-__________------- ___ 8<br />

Devonian:<br />

Pegram limestone (Sellersburg formation) Dark-<br />

brown semicrystalline limestone carrying numerous<br />

large heliophylloid corals, becoming purer gray below<br />

and very conglomeratic (semiedgewise) near base. _ About 4<br />

Pegram limestone (Jeffersonville formation) White,<br />

brown, or pink coarse sugary sandstone, very f ossilif er-<br />

ous at top; barren and exhibiting extremely unsettled<br />

conditions of deposition in lower 4 feet. Fauna: Lep-<br />

taena rhomboidalis, Stropheodonta aff. S. hemispherica,<br />

Stropheodonta demissa, Leptostrophia aff. L. perplana,<br />

Schuchertella sp., Spirifer cf. S. varicosus, Cystodictya<br />

gilberti, Fenestella sp., Rhipidomella aff. R. vanuxemi,<br />

Hadrophyllum orbignyi, Chonetes aff. C. mucronatus,<br />

Centronella? glansflagae cf. Pholidostrophia iowensis,<br />

Polypora sp., Loculipora sp., Cystodictya sp., Anibo-<br />

coelia sp., crinoid stems__________________________ 9<br />

Silurian: Niagaran. Formation undetermined.<br />

« Foerste, A. F., op. cit. (1901), pp. 425-426.<br />

w Dunbar, C. 0., op. cit., p. 91.<br />

» Pohl, E. R., personal communication, February 6,1929.

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