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Subsection M262Bh
Upper San Gorgonio Mountains

This subsection comprises the higher elevations and cooler parts of the San Bernardino Mountains.  The climate is temperate to cold, and subhumid.  MLRA 22d.
 

Lithology and Stratigraphy.  This subsection contains mostly Mesozoic granitic rocks.  Also, there are some Pre-Cambrian gneiss and Paleozoic marine sedimentary rocks. The mountains are a horst with faults and steep escarpments on the south-southwest, east-northeast, and west-northwest sides.  Quaternary nonmarine sediments and Recent alluvium are small but important components of the subsection.

Geomorphology.  This is a subsection of steep and very steep mountains with narrow to rounded summits.  There is  a high rolling plateau surface at about 6500 to 7500 feet with some Quaternary fluvial and lacustrine deposits on it. The subsection elevation range is from about 4000 feet up to 11,502 feet on Mount San Gorgonio.  Mass wasting and fluvial erosion are the main geomorphic processes.

Soils.  The soils are mostly shallow Typic Xeropsamments, Typic Xerochrepts, Pachic Xerumbrepts, and Ultic Argixerolls. Also, there are Mollic Xerofluvents on late Quaternary alluvium.  The soils are leached free of carbonates.  The soils are well drained.  Soil temperature regimes are mostly mesic, and some frigid at higher elevations.  Soil moisture regimes are xeric.

Vegetation.  The predominant natural plant community is Ponderosa pine series.  There are small areas of Coulter pine series, Mixed chaparral shrublands, Jeffrey pine series on the north side of the mountains, and small areas of Limber pine series.  Lodgepole pine series is common at higher elevations.

Climate.  The mean annual precipitation is about 30 to 40  inches.  Much of it is snow.  Mean annual temperature is about 40° to 50°  F.  The mean freeze-free period is about 150 to 200 days.

Surface Water.  Runoff is rapid.  All but the larger streams are dry through the summer.  There have been natural lakes on the high plateau recently, but any lakes that persisted until historical time have been replaced by reservoirs. 


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