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Wavelike movement of bedload sediment, East Fork River, Wyoming

Environmental Geology and Water Sciences

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DOI: 10.1007/BF02509922

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Abstract

Bedload is moved down the East Fork River in distinct wavelike pulses that have the form of composite dune fields The moving material consists mostly of coarse sand and fine gravel The wavelengths of the pulses are about 500-600 m, a distance that is predetermined by the pattern of stoage of bed sediment in the river during low water As the river discharge increases, the bed sediment is scoured from the storage areas, and it is moved onto and across the interventing riffles As the river discharge decreases, the bed sediment is scoured off the riffles and moved into the next storage area downstream Each successive pulse of water discharge sets into motion a wave of bedload that continues to move unitil it reaches the next storage area ?? 1985 Springer-Verlag New York Inc.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Wavelike movement of bedload sediment, East Fork River, Wyoming
Series title:
Environmental Geology and Water Sciences
DOI:
10.1007/BF02509922
Volume
7
Issue:
4
Year Published:
1985
Language:
English
Publisher location:
Springer-Verlag
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
First page:
215
Last page:
225
Number of Pages:
11