| Subsection map Ecological Section map Previous Subsection Next Subsection |
Lithology and Stratigraphy. This subsection is dominated by Jurassic and Cretaceous Franciscan sedimentary, minor volcanic, and metamorphic rocks of the Central Belt; some Franciscan rocks of the Coastal Belt are present. They are intensely folded and faulted. There are small areas of Tertiary marine sedimentary rocks and ultramafic rocks are sparsely scattered through the Franciscan Complex.
Geomorphology.
This is a subsection of mountains with rounded ridges, steep and moderately
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. Larabee Valley along
the Van Duzen River is wide enough to have an appreciable alluvial plain.
The subsection elevation range is from sea-level up to 4408 feet on Showers
Mountain. Mass wasting and fluvial erosion are the main geomorphic
processes.
Soils.
The soils are mostly Typic Humitropepts and Mollic Hapudalfs in the northern
one-third of the subsection. They are predominantly Dystric Xerochrepts
and Haploxeralfs in the southern two-thirds of the subsection, and less
extensive Ultic Argixerolls. The soils are leached free of carbonates,
with the possible exception of some Argixerolls, and the older ones in
the northern part of the subsection are strongly acid. The soil temperature
regimes are predominantly isomesic in the northern one-third and mesic
in the southern two-thirds of the subsection. Soils in grassland
in the southern part of the subsection have thermic soil temperature regimes.
Soil moisture regimes are predominantly udic and xeric (near udic).
Vegetation. The predominant natural plant communities are Redwood series in the northern one-third and Douglas-fir - tanoak series in the southern two-thirds of the subsection. Needlegrass grasslands are common in the southern part of the subsection, and Oregon white oak series is also common. Common in riparian areas are Red alder series in the northern part and Black cottonwood series in the southern part of the subsection.
Surface Water. Runoff is rapid and many of the smaller
streams are dry by the end of the summer. Natural lakes are
absent.
| Subsection map Ecological Section map Previous Subsection Next Subsection |