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Lithology and Stratigraphy. This subsection is dominated by Jurassic and Cretaceous Franciscan metaclastic rocks of the Eastern Belt. They are intensely folded and faulted. Ultramafic rocks are minor components in this subsection.
Geomorphology.
This is a subsection of mountains with rounded ridges, steep sides,
and narrow canyons. Most of the mountains are elongated
in north-northwest to northwest directions and have subequal summits with
increasing elevation toward the interior. The elevation range
is from about 1200 feet up to 8092 feet on Mt. Linn in the South Yolla
Bolly Mountains. Mass wasting and fluvial erosion are the main geomorphic
processes.
Soils.
The soils are mostly Dystric Xerochrepts, Dystric Lithic Xerochrepts, and
Lithic Xerorthents. At higher elevations, Typic and Lithic Xerumbrepts
are most common. The soils are leached free of carbonates.
Few surfaces are old enough, because of active erosion, to have Alfisols
or Ultisols. Soil temperature regimes are predominantly mesic, some
frigid, and minor cryic. Soil moisture regimes are almost exclusively
xeric.
Vegetation. The predominant natural plant community is Mixed conifer series, except in the northern part of the subsection where Douglas-fir - tanoak series is the predominant plant community. Red fir series and White fir series are common in areas of frigid soil temperature regimes.
Characteristic series by lifeform include:
Surface Water. Runoff is rapid and all but the larger streams
are dry through much of the summer. There are a few small lakes and
wet meadows in glacial basins at higher elevations.
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