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・ California Citrus State Historic Park
・ California City Municipal Airport
・ California City, California
・ California Civil Code
・ California Civil War Confederate Units
・ California Clam Chowder
・ California Clay Movement
・ California Climate Action Registry
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California Coast Ranges
・ California Coast University
・ California Coastal Commission
・ California Coastal Conservancy
・ California Coastal National Monument
・ California Coastal National Monument Expansion Act of 2013
・ California coastal prairie
・ California Coastal Records Project
・ California coastal sage and chaparral ecoregion
・ California coastal salt marsh
・ California Coastal Trail
・ California Code of Civil Procedure
・ California Code of Regulations
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・ California College of Ayurveda


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California Coast Ranges : ウィキペディア英語版
California Coast Ranges

The Coast Ranges of California span from Humboldt County, California south to Santa Barbara County. The other three coastal California mountain ranges are the Transverse Ranges, Peninsular Ranges and the Klamath Mountains.〔
Physiographically, they are a section of the larger Pacific Border province, which in turn are part of the larger Pacific Mountain System physiographic division. UNESCO has included the "California Coast Ranges Biosphere Reserve" in its Man and the Biosphere Programme of World Network of Biosphere Reserves since 1983.
==Physiography==

The northern end of the California Coast Ranges overlap the southern end of the Klamath Mountains for approximately 80 miles on the west. They extend southward for more than 600 miles to where the coastline turns eastward along the Santa Barbara Channel, around the area of Point Conception. Here the southern end meets the Los Angeles Transverse Ranges, or (Sierras de los Angeles). The rocks themselves that comprise the mountains are of a great variety and widely varying geologic ages. Most of the rocks were formed during the Tertiary, Cretaceous and Jurassic periods. Most were deposited on the sea bottom as sediments, but in many places also had the cracks, crevices and other gaps infused with molten lava or other masses of igneous rock, which were forced in molten condition into the sedimentary rocks. All of the range has been folded and faulted during several periods, with erosion of the softer rock giving much of the current appearance.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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