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Basal sandstone of the Oil Creek Formation in the quarry of the Pennsylvania Glass Sand Corporation, Johnston County, Oklahoma

By
J. G. McPherson
J. G. McPherson
Mobil Research and Development Corporation, Dallas Research Laboratory, P.O. Box 819047, Dallas, Texas 75381
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R. E. Denisen
R. E. Denisen
Mobil Research and Development Corporation, Dallas Research Laboratory, P.O. Box 819047, Dallas, Texas 75381
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D. W. Kirkland
D. W. Kirkland
Mobil Research and Development Corporation, Dallas Research Laboratory, P.O. Box 819047, Dallas, Texas 75381
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D. M. Summers
D. M. Summers
Mobil Research and Development Corporation, Dallas Research Laboratory, P.O. Box 819047, Dallas, Texas 75381
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Published:
January 01, 1988

Abstract

The basal sandstone of the Oil Creek Formation is well exposed in a quarry located 5 mi (8 km) north northwest of the small town of Mill Creek in Johnston County, Oklahoma (Sec.14, T.1S., R4E.) (Figs. 1 and 2). The quarry is owned by the Pennsylvania Glass Sand Corporation and is about 0.5 mi (0.8 km) west of Oklahoma 7, which passes through Mill Creek and connects with I-35 about 20 mi (32 km) to the west.

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Contents

DNAG, Centennial Field Guides

South-Central Section of the Geological Society of America

O. T. Hayward
O. T. Hayward
Geology Department, Baylor University, Waco, Texas 76798
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Geological Society of America
Volume
4
ISBN electronic:
9780813754109
Publication date:
January 01, 1988

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