Sierra Madre (California)

Geography

The Sierra Madre range trends from northwest to southeast, and is approximately 25 mi long. High peaks in the range include McPherson Peak at 5747 ft in elevation, and the highest point in the range, Peak Mountain at 5843 ft in elevation. Snow falls on the higher elevations during the winter months.

The range forms the southwestern side of the Cuyama Valley. The La Panza Range is a northern extension of the Sierra Madre, located in eastern San Luis Obispo County.

The Sierra Madre is almost entirely within the Los Padres National Forest, and marks the northern boundary of the San Rafael Wilderness area. The southeastern extent of the range is about 25 mi north of the city of Santa Barbara, and the northwestern extent of the range is about 50 mi north by northwest of the city.

To the southeast, the range merges with the San Rafael Mountains of the Transverse Ranges System, in a complex topography of unnamed ranges. The adjacent highest point of the San Rafael Mountains, and in all Santa Barbara County, is Big Pine Mountain (6820 ft).

Natural history

The Sierra Madre lies in the region historically inhabited by the Chumash people, who used sites in the mountains for sacred ceremonies and rites. Numerous petroglyphs can still be found in the area, including the Painted Rock Site, identified as S'ap'aski or House of the Sun in Chumash tradition.

The predominant vegetation type on the mountains is chaparral shrubland, with oak woodlands that occur in microclimates, both of the California interior chaparral and woodlands sub-ecoregion. The higher elevations support California mixed evergreen forest and small areas of coniferous forest habitats.

The mountains are one of the most important undeveloped habitat areas of the endangered California condor.

Geologically, the mountains are mostly sedimentary rock of Tertiary age, with some marine and non-marine sedimentary rocks of Eocene and Upper Cretaceous age. There is a large proportion of sandstone, and one region in the eastern portion of the range is made up of Neogene sediments.

The mountain range is almost entirely uninhabited, except for portions of the lower slopes to the north, which have been developed for oil and gas production at the South Cuyama Oil Field. One difficult, single-lane dirt road follows the mountain crest; it often is closed after storms, and is normally only passable by four-wheel-drive vehicles or motorcycles.

References

References

1. {{Cite gnis
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3. Cliff, Edward P. (Chairman). (1965). "Decisions on Geographic Names in the United States". [[United States Department of the Interior]].
4. Fairbanks, Harold W.. (1901). "The Physiography of California". Jones & Kroeger Printers.
5. (1978). "The Painted Rock Site (SBa-502 and SBa-526): Sapaski, the House of the Sun". Journal of California Anthropology.
6. "Dan McCaslin: The Glories of Sierra Madre Ridge and the Cuyama".
7. "California Vegetation - WHR13 Types". California National Resources Agency.
8. Frederiksen, Norman O.. (1985). ""Map showing thermal-alteration indices in roadless areas and the Santa Lucia Wilderness in the Los Padres National Forest, southwestern California"". U.S. Geological Survey.