Research Article
Jan 1951
Origin and Significance of Openwork Gravel
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VIEW THE REPLYPublication: Transactions of the American Society of Civil Engineers
Volume 116, Issue 1
Abstract
Openwork gravel, without interstitial sand, is found associated with stream deposits of well-graded sand and gravel in innumerable exposures throughout the Pacific Northwest. A study of the relationships suggests that. openwork gravel is deposited by swift streams on the downstream face of a gravel bar or as sloping beds on a delta face. Vortex action may be partly responsible for the absence of sand in the deposit. Openwork gravel is of significance in engineering works involving water because of its common occurrence, the usual lenticular shape of a deposit, and its extremely high permeability.
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© 1951 American Society of Civil Engineers.
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Published in print: Jan 1951
Published online: Feb 10, 2021
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Allen S. Cary, AM.ASCE
Senior Geologist, Seattle Dist., Corps of Engrs., Dept. of the Army, Seattle, Wash.
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Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.
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