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Lithology and Stratigraphy. This subsection contains mostly Mesozoic granitic, gabbroic, marine (Jurassic) sedimentary, and metavolcanic rocks in the hills. The valleys are filled with Quaternary alluvium.
Geomorphology. This subsection is on moderately steep to
steep hills, pediments, dissected Quaternary nonmarine sediments adjacent
to the Elsinore Fault Zone and near the Santa Ana River, and Recent alluvium
in Perris Valley and along the Elsinore Fault Zone. The subsection
elevation range is from about 1400 feet to 2600 feet. Mass wasting
and fluvial erosion and deposition are the main geomorphic processes.
Soils. The soils are mostly shallow Typic Xerorthents and
Typic Haploxeralfs on hills and pediments in granitic terrain and
Lithic Haploxerolls, Mollic Haploxeralfs, and Typic Natrixeralfs on other
hills. On Recent alluvium, there are Typic Xerofluvents, Fluventic
and Fluvaquentic Haploxerolls. There are Natric Haploxeralfs, Haplic
and Typic Durixeralfs, and Typic Pelloxererts on dissected nonmarine Quaternary
deposits and terraces. Carbonates have accumulated in some of the
soils and silica has accumulated in the older soils. The soils are
well drained, except for somewhat poorly drained Fluvaquentic Haploxerolls
in Recent alluvium. Soil temperature regimes are thermic, and soil
moisture regimes are xeric.
Vegetation. The predominant natural plant communities are California sagebrush - California buckwheat series and Needlegrass grasslands. There is some Black sage series and small areas of Coast live oak series and Chamise series.
Surface Water. Runoff is rapid, except from floodplains and lake basins. All but the larger streams are dry through the summer. There are sag ponds along the Elsinore Fault Zone, Lake Elsinore being the largest. Also, there are several reservoirs in the subsection.
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