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Lithology and Stratigraphy. Mesozoic granitic rocks predominate in this subsection. Also, there are Paleozoic marine sedimentary and metavolcanic rocks. Quaternary alluvium and glacial till are present, but not extensive.
Geomorphology. This subsection is on a gently sloping to moderately steep plateau that is bisected by the North Fork of the Feather River. The North Fork has cut across the plateau and runs in the bottom of a very steep sided canyon, about 2000 to 4000 feet below the plateau surface. Higher parts of the plateau and the northern edge of it were glaciated during the Pleistocene. The elevation ranges from about 2000 feet along Feather River up to 7176 feet on Bald Eagle Hill. Fluvial erosion and, in the Feather River canyon, mass wasting are the main geomorphic processes.
Soils. The soils on granitic rocks are mostly Dystric, Lithic, and shallow Typic Xeropsamments and Typic and Dystric Xerochrepts. On other kinds of rocks they are mostly Dystric Xerochrepts; Andic Xerumbrepts; Lithic Ultic and Ultic Haploxerolls; and Ultic Haploxeralfs. The soils are well drained. Soil temperature regimes are frigid on the plateau and mostly mesic in the canyon of the Feather River. Soil moisture regimes are mostly xeric.
Vegetation. The predominant natural plant communities are Mixed conifer series and White fir series. Jeffrey pine series is common in glacially eroded, or scoured, terrain. There is some Red fir series at higher elevations. Huckleberry oak series occurs on very stony colluvium, or talus. Wet areas with Sedge meadow communities and Mountain alder series or Lodgepole pine series are common, but not extensive.
Surface Water. Runoff is rapid from most of the area. Most of the runoff flows to the North Fork of the Feather River or its tributaries. There are some small lakes, or ponds, in the glaciated terrain, and a large reservoir (Bucks Lake).
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