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Lithology and Stratigraphy. Mesozoic granitic rocks and Jurassic - Triassic metavolcanic rocks are most extensive in this subsection. Paleozoic marine sedimentary, ultramafic, and mafic plutonic rocks are moderately extensive. There are small areas of basalt and andesite in the northern part of the subsection, and andesitic lahar along the southeastern edge of the subsection. Quaternary alluvium and glacial till are present, but not extensive.
Geomorphology.
This subsection is on a gently sloping to moderately steep plateau that
is crossed by the North, Middle, and South Forks of the Feather River and
the North Yuba, Middle Yuba, and South Yuba Rivers. These rivers
run in the bottom of very steep sided canyons that are as much as 2000
feet below the plateau surface. The elevation ranges from about 1000
feet up to 6095 feet on Table Mountain, but most of the rolling plateau
is below 5000 feet in this subsection. Fluvial erosion and, in the
river canyons, mass wasting are the main geomorphic processes.
Soils. The soils are mostly Typic, Dystric, and shallow Dystric Xerochrepts; Mollic and Ultic Haploxeralfs; Lithic Xeropsamments; and shallow Entic Haploxerolls on granitic rocks; plus Typic Haploxerults; Xeric Haplohumults; Lithic and Dystric Lithic Xerochrepts; and Ultic Palexeralfs on other kinds of rocks. The soils are well drained. Soil temperature regimes are mostly mesic. Soil moisture regimes are xeric.
Vegetation. The predominant natural plant community is Mixed conifer series. Douglas-fir - tanoak series is common in areas of greater precipitation. There is some Ponderosa pine series at lower elevations, Canyon live oak series on very steep, rocky canyon sideslopes, and Mixed chaparral shrublands on steep south-facing slopes with shallow soils.
Surface Water. Runoff is rapid from most of the area. Most of the runoff flows to the Feather River or Yuba River or tributaries of them. There are no natural lakes, but some reservoirs.
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