Definitions
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Examples
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In granitic terrain of Montara Mountain the soils are mostly Lithic and Typic Haplu-stolls and Pachic Argixerolls.
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Typic Natrixeralfs and Ultic Palexerolls are present on nonmarine terraces on the Monterey Peninsula.
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Typic Xeropsamments, Psammentic Haploxerolls, and Alfic Xeropsamments are the main soils on dunes.
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On Tertiary marine and Plio-Pleistocene nonmarine sediments, they are mostly Xerorthents, Typic Haploxeralfs, and Typic Argixerolls.
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The main soils are mostly Typic Chromoxererts and Typic Chromusterts on volcanic rocks; Lithic, and Mollic Haploxeralfs of rocks of the Franciscan formation; Mollic Haploxeralfs, and Typic Natrustalfs on Eocene sedimentary rocks.
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Typic Xeropsamments are common on stabilized dunes.
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The soils are mostly Fluventic, Fluvaquentic, and Pachic Haploxerolls and Typic and Chromic Pelloxererts on floodplains.
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They are Entic, Typic, and Pachic Haploxerolls, Ultic Palexerolls, and Typic Natrixeralfs on stream terraces and old alluvial fans.
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Typic Argixerolls, Mollic Haploxeralfs, and Abruptic Durixeralfs are common on alluvial fans and terraces.
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Typic and Alfic Xeropsamments prevail in eolian sand behind beaches and on some marine terraces.
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