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Dick Smith Wilderness
The Dick Smith Wilderness is a wilderness area in the mountains of eastern Santa Barbara County, California, USA, with a portion in Ventura County. It is completely contained within the Los Padres National Forest, and is northeast of the city of Santa Barbara and north of the city of Ojai. It is most easily accessible from two trailheads off State Route 33, which runs north from Ojai. It is adjacent to the large San Rafael Wilderness on the west and the Matilija Wilderness on the south. Across Highway 33 to the east, and also in the Los Padres National Forest, is the large Sespe Wilderness.
The wilderness is named after Santa Barbaran Dick Smith, who was a reporter, photographer, historian and pioneer in environmental journalism for the ''Santa Barbara News-Press''. Smith spent more times in these remote regions of Santa Barbara County than anyone, covering the area on horseback and accompanied by his dog. In recognition of Dick's personal pursuit to preserve the wild back country the area was named in his honor, and the U.S. Congress created the wilderness in 1984 as part of the California Wilderness Act.〔From the Dick Smith Wilderness description page at the Los Padres National Forest web site ()〕
==Geography==
The wilderness is in the Transverse Ranges, east of the junction of the San Rafael Mountains and Sierra Madre Mountains at Big Pine Mountain. Madulce Peak, at 6,541 feet, is the highest mountain completely within the wilderness, and the lowest point is 3,700 feet where Santa Barbara Creek exits to the north. The wilderness contains the divide between two watersheds: the Cuyama River to the north, and the Santa Ynez River to the south. The major streams carrying runoff to those two rivers are Santa Barbara Creek and Mono Creek, respectively.
The Big Pine Fault cuts through the wilderness from west to east, trending northeast after exiting the wilderness, in the direction of the nearby San Andreas Fault, which is only about 12 miles from the wilderness boundary. The Pine Mountain Fault splits off from the Big Pine; it is visible along the southern slope of nearby Reyes Peak. Most rocks in the wilderness are Eocene marine sediments, with some scattered outcrops of Pliocene, Miocene, and Oligocene sediments, especially immediately to the south of the Pine Mountain Fault (the contact between these rock units and the Eocene sediments defines the Big Pine Fault).〔Jennings/Strand, Geologic Map of California, Los Angeles Sheet (1:250,000 scale).〕
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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