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Raised Submarine Canyons

An Exploratory Hypothesis

Bibliographic Data

ID8376455
AuthorsJOHN H WINSLOW (corresponding author)
Year1966
Volume56
Issue4
Pages634-672
Publication date1966-12-01
Open AccessNo
TypeARTICLE
VenueAnnals of the Association of American Geographers (JOURNAL)
Journal identifiersISSN: 0004-5608 • E-ISSN: 1467-8306
PublisherInforma UK Limited (PUBLISHER • GB)
DOI10.1111/j.1467-8306.1966.tb00583.x
OpenAlexW1973455305
LanguageEN
Citations received1
References cited35

Submarine canyons are now widely believed to have been eroded by submarine processes, possibly turbidity currents. Although they may resemble, in a general way, the typical subaerially eroded land valleys, they also possess distinct characteristics of their own. Regions that have emerged from beneath the ocean since, or possibly prior to, the mid-Tertiary might still have relict submarine canyons on their surfaces. Enigmatic coastal indentations, such as certain fjords, estuaries, rias, and lagoons, together with some dry and underfit stream valleys, may be of this origin. Many bear a resemblance to submarine canyons and some appear to be linked with present canyons on the continental shelves. A number of problems that have been part of conventional interpretations of their origin are resolved by this hypothesis; a few new problems, it must be admitted, are created

Canyon · Continental shelf · Fjord · Geography · Geomorphology · Sedimentary depositional environment · Structural basin · Submarine · Submarine canyon · Turbidity current · Geological formations and processes · Geology · Geology and Paleoclimatology Research · Maritime and Coastal Archaeology · Oceanography · Paleontology

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    Open Access•Francis P Shepard, Charles N Beard•Geographical Review•1938

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    Open Access•Francis P Shepard•Geographical Review•1933

Citations per year0.08
Citation span2013 - 2013 (1)
Highly citedNo

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