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Studies of fluctuations in amount of sand on beaches and adjacent shallow sea floors of Southern California together with variations in wave size and type prove direct relationship exists between these phenomena; theoretical studies of oscillatory waves prove existence of mass transport of water and field and laboratory investigations confirm water movement; explanation given accounts for fluctuation in amount of sand on beach and variation in grain size.
Studies of fluctuations in amount of sand on beaches and adjacent shallow sea floors of Southern California together with variations in wave size and type prove direct relationship exists between these phenomena; theoretical studies of oscillatory waves prove existence of mass transport of water and field and laboratory investigations confirm water movement; explanation given accounts for fluctuation in amount of sand on beach and variation in grain size.
Waves as sand-transporting agent
Am J Sci
Grant, U.S. (Autor:in)
1943
7 pages
Aufsatz (Zeitschrift)
Englisch
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