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The Quaternary Deltaic and Channel System in the Central Great Valley, California

Bibliographic Data

ID8376545
AuthorsRoy J Shlemon (University of California, Davis, corresponding author)
Year1971
Volume61
Issue3
Pages427-440
Publication date1971-09-01
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.1467-8306.1971.tb00797.x
OpenAlexW2048906850
LanguageEN
Citations received4
References cited8

Three and possibly four Mokelumne River fan deposits and gravel-filled channels interfinger deltaic sediments in the central part of the Great Valley of California. The channels were probably cut during successive glaciations in the Sierra Nevada Mountains, and graded to eustatically lowered and possibly subsiding base levels. Rising seas caused thalassostatic sedimentation and headward expansion of the California Delta during interglacial time. Radiocarbon dating of basal deltaic peat indicates the Pleistocene-Holocene transition occurred about 10, 700 years ago in this part of California

Archaeology · Channel (broadcasting) · Delta · Geography · Geomorphology · Holocene · Interglacial · Peat · Physical geography · Pleistocene · Quaternary · Radiocarbon dating · Coastal wetland ecosystem dynamics · Geological formations and processes · Geology · Geology and Paleoclimatology Research · Paleontology

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Citations per year0.08
Citation span1976 - 2024 (49)
Highly citedNo

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