Geology of the Bedford Shale and Berea Sandstone in the Appalachian Basin

Pepper, James F.; Witt, Wallace De; Demarest, David P.

doi:10.1126/science.119.3094.512-b

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Devonian Outcrop1

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1985

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“…The Chattanooga with its two members, the Dowelltown and the Gassaway, is present in much of the subsurface of Tennessee. Locally the Dowelltown is absent by nondeposition on shoal areas in the Chattanooga Sea (Conant and Swanson, 1961, p. 18 (Pepper, de Witt, and Demarest, 1954). It underlies much of eastern Ohio, western West Virginia, and eastern Kentucky.…”

Section: Devonian Outcropmentioning

confidence: 99%

Stratigraphic notes, 1984

1985

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The San Pablo Formation is geographically restricted from the area south of Hospital Creek on the east flank of the Diablo Range.Strata previously assigned to the basal part of the San Pablo Formation and lower previously unnamed strata are herein reassigned to the Poverty Flat Sandstone (new) of late middle and late Eocene age.The Valley Springs Formation (upper Oligocene and lower Miocene) is extended from the east side of the northern San Joaquin Valley to include part of the original San Pablo Formation. The remainder of the strata previously assigned to the San Pablo Formation are reassigned to the Neroly Sandstone (upper Miocene).

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Section: Devonian Outcropmentioning

confidence: 99%

Stratigraphic notes, 1984

1985

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Geology of the Bedford Shale and Berea Sandstone in the Appalachian Basin

Cited by 1 publication

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Stratigraphic notes, 1984

Stratigraphic notes, 1984

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