1950
DOI: 10.3133/pp230
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Geology of the Elkton area, Virginia

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Cited by 29 publications
(42 citation statements)
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“…East of the Allegheny structural front, the basal sandstone unit and the Shady Dolomite interval presumably correlate with the uppermost part of the Lower Cambrian Chilhowee Group and the Lower Cambrian Shady Dolomite that crops out in northern Virginia between the North Mountain fault and the Blue Ridge, respectively (figs. 1, 2) (Butts, 1940;King, 1950;Brent, 1960;Rader, 1982).…”
Section: Basal Sandstone Unit and Shady Dolomite (Lower Cambrian)mentioning
confidence: 99%
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“…East of the Allegheny structural front, the basal sandstone unit and the Shady Dolomite interval presumably correlate with the uppermost part of the Lower Cambrian Chilhowee Group and the Lower Cambrian Shady Dolomite that crops out in northern Virginia between the North Mountain fault and the Blue Ridge, respectively (figs. 1, 2) (Butts, 1940;King, 1950;Brent, 1960;Rader, 1982).…”
Section: Basal Sandstone Unit and Shady Dolomite (Lower Cambrian)mentioning
confidence: 99%
“…1) and (2) published outcrop descriptions of the Rome and Waynesboro Formations in northern Virginia between the North Mountain fault and the Blue Ridge (King, 1950;Edmundson and Nunan, 1973;Gathright and Nystrom, 1974). These data suggest that, east of the Rome trough, the Rome Formation and equivalent units thin abruptly across the Central West Virginia arch before they thicken eastward to an estimated 1,600 ft near the Allegheny structural front (pi.…”
Section: Rome Formation (Lower and Middle Cambrian)mentioning
confidence: 99%
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