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GEOREF RECORD

Submarine abrasion and wave-cut platforms [California]

William Crane Bradley
Submarine abrasion and wave-cut platforms [California]
Bulletin of the Geological Society of America (August 1958) 69 (8): 967-974

Abstract

According to classical theory, wave-cut platforms are developed by deep submarine abrasion while sea level is stationary. Modern writers, however, believe that wave erosion takes place only in shallow water. Fragile, subaerially etched pyroxene sand grains are mechanically unstable at depths of less than about 30 feet in the Santa Cruz area of California but are mechanically stable at greater depths, supporting the conclusion that significant wave-produced submarine abrasion is restricted to the surf zone with a maximum depth of about 30 feet. Most sediment in transit beyond the surf zone is too fine-grained to act as an abrasive. If sea level is stationary, marine planation may produce a wave-cut platform up to about one-third of a mile wide; a wider platform can be cut only during slow submergence. The modern and former platforms in the Santa Cruz area were carved while sea level was rising.


ISSN: 1050-9747
Coden: BUGMAF
Serial Title: Bulletin of the Geological Society of America
Serial Volume: 69
Serial Issue: 8
Title: Submarine abrasion and wave-cut platforms [California]
Pages: 967-974
Published: 195808
Text Language: English
Publisher: Geological Society of America (GSA), Boulder, CO, United States
Accession Number: 1959-043986
Categories: OceanographyGeomorphology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus.
N32°30'00" - N42°00'00", W124°30'00" - W114°15'00"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2019, American Geosciences Institute. Reference includes data from Bibliography and Index of North American Geology, U. S. Geological Survey, Reston, VA, United States
Update Code: 1959
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