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Abstract
Geology and Tectonics of the Central California Coast Region - San Francisco to Monterey, 1990
Pages 185-191
Quaternary Geology of the Monterey Bay Region, California
William R. Dupre
Abstract
The central Monterey Bay region (Figure 1) has been a stable to subsiding depocenter and the locus of fluvial, alluvialfan, and eollan activity throughout the Quaternary. It and adjacent tectonically uplifting areas provide an opportunity to study the development of marine and non-marine depositional systems as a function of fluctuating sea level and tectonic setting.
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