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Lithology and Stratigraphy. This subsection contains mostly Mesozoic granitic rocks and Pre-Cambrian anorthosite. Also, there is some Pre-Cretaceous Pelona schist.
Geomorphology. This is a subsection of steep and very steep mountains with narrow to rounded summits and narrow canyons. The mountains trend east-west, but hills along the San Andreas fault trend west-northwest. The subsection elevation range is from about 500 feet up to 6000 feet. Mass wasting and fluvial erosion are the main geomorphic processes.
Soils. The soils are mostly Lithic and shallow Typic Xerorthents, shallow Entic Haploxerolls, and Calcic Haploxerolls. Most of the soils, but not all, are leached free of carbonates. The soils are well drained. Soil temperature regimes are mostly thermic, and some mesic on north-facing slopes at higher elevations. Soil moisture regimes are xeric.
Vegetation. The predominant natural plant communities are Chamise series and Chamise - hoaryleaf ceanothus series, which are generally on shallow and very stony soils. Live oak chaparral series and Mixed chaparral shrublands also occur. Ponderosa pine series with some Bigcone Douglas-fir series and Bigcone Douglas-fir - canyon live oak series occurs on north-facing slopes, Jeffrey pine series occurs on the north-northeast side of the mountains, and California juniper series occurs on hills along the San Andreas fault.
Surface Water. Runoff is rapid. All but the larger streams are dry through the summer. Natural lakes are absent, except along the San Andreas fault. There are some sag ponds along the San Andreas fault.
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