| Subsection map Ecological Section map Previous Subsection Next Subsection |
Lithology and Stratigraphy. This subsection contains mostly Mesozoic granitic rocks, with large areas of Pliocene and Pleistocene nonmarine sediments and Recent alluvium. Also, there are Pre-Cretaceous granitic, marine (Jurassic) sedimentary, and metamorphic rocks.
Geomorphology. This subsection is on lower mountain slopes, moderately steep to steep hills, and nearly level to gently sloping alluvial plains in Terwilliger Valley and other small valleys. There are alluvial fans, terraces, and floodplains on the alluvial plains. Pliocene and some Pleistocene nonmarine sediments along the San Jacinto Fault northwest of the Cahuilla Mountains have been eroded to badlands. The subsection elevation range is from about 1500 feet to 4000 feet. Mass wasting and fluvial erosion and deposition are the main geomorphic processes.
Soils. The soils on granitic rocks are mostly shallow Typic Xerorthents, Typic Xerochrepts, and Typic Haploxeralfs at lower elevations and shallow Entic Haploxerolls, Entic Ultic Haploxerolls, and Mollic Haploxeralfs at higher elevations. There are Lithic Haploxerolls and Typic Natrixeralfs on other kinds of rocks. Soils in badlands are Xerorthents. Haploxerolls predominate in Recent alluvium. Calcium carbonates have accumulated in some of the soils at lower elevations. The soils are well drained. Soil temperature regimes are mostly thermic; and soil moisture regimes are xeric.
Vegetation. The predominant natural plant communities are Coast Live oak series, California sagebrush - California buckwheat series, and Black sage series at lower elevations southwest of the San Jacinto Fault, and some Chamise series and Red shank - chamise series.
Surface Water. Runoff is rapid, except from nearly level alluvial plains. All but the larger streams are dry through the summer. There are no natural lakes.
| Subsection map Ecological Section map Previous Subsection Next Subsection |