Everything about The San Rafael Wilderness totally explained
The
San Rafael Wilderness is a wilderness area in the mountains of north central
Santa Barbara County,
California,
USA. It is completely contained within the
Los Padres National Forest, and is north of the city of
Santa Barbara and east of
Santa Maria. Formed in 1968, it was the first wilderness area to be created from a previously designated
Primitive Area after the passage of the 1964
Wilderness Act. It also includes the Sisquoc
Condor Sanctuary, created in 1937, which is the oldest designated sanctuary for the large
endangered birds.
Geography
Most of the wilderness lies between the crests of two parallel mountain ranges, the
San Rafael Mountains and
Sierra Madre Mountains, and includes the drainages of two watercourses: the Sisquoc River and Manzana Creek. Both flow to the northwest, eventually joining together and draining into the ocean near Santa Maria. Elevations within the wilderness vary from at the confluence of Manzana Creek and the Sisquoc River on the western boundary, to over 6,800 feet at
Big Pine Mountain, the highest point in Santa Barbara County. Dividing the drainages of the Manzana and Sisquoc is a ridge known as Hurricane Deck, a rugged 15 mile slab of upthrust
sandstone with a trail snaking along the top.
Rock formations in the wilderness are predominantly
sedimentary, and are of
Miocene and
Cretaceous age. Both the Nacimiento and Big Pine Faults run through the wilderness, roughly parallelling the Sierra Madre and San Rafael Mountain crests respectively. Hurricane Deck is a single block of Miocene-age sedimentary rock. Immediately south of the wilderness, opposite the Big Pine and Camuesa Faults, is a large region of the
Franciscan Formation.
Mercury was formerly mined in this area, and abandoned mines along with tailings piles can be found.
Climate
The climate of the wilderness is
Mediterranean, although the distance from the coast allows for cooler winters and hotter summers than are found in the coastal strip. Snow is common on the higher peaks in the winter, although it rarely lingers except on north-facing slopes. Rain is extremely rare in the summer, and dry lightning from the occasional thunderstorms can start fires.
Vegetation and wildlife
The typical vegetation in the wilderness is
chaparral and
oak woodland, although there are stands of pine and fir at higher elevations and on north-facing slopes, as well as
riparian forests in the streams. The river valleys open out in a few places to allow for meadows and
grasslands; these are the locations that were settled in the 19th century. Wildlife that may be encountered in the wilderness includes coyotes, black bears, and mountain lions. The California Condor can occasionally be seen, since the endangered bird was released back into the wild in 1992. The 1200 acre Sisquoc Condor Sanctuary, in the southeastern part of the wilderness, was chosen for its inaccessible terrain, which includes rock ledges favored by condors for nesting sites. Public entry is prohibited in the Sanctuary.
History
The region has been continuously inhabited by humans for over 10,000 years. Rock art by the resident
Chumash Indians is scattered across the region; locations of rock paintings are generally not made public for fear of vandalism.
In the 1880s, a group of about 200
faith healers, lead by
Hiram Preserved Wheat (1822–1903), settled along the Sisquoc River in about 20 separate homesteads. The ruins of their habitations, including the "Manzana Schoolhouse," can be seen to the present day. At the time, they were mistakenly called "
Mormons," and the error has been preserved in the name of one campsite along the Sisquoc River in the central part of the wilderness. They built the schoolhouse in 1893, but by 1902 it was closed, and most of the group had left. After the faith healers had left, another settler, Charles Dabney, built a cabin for himself and his family in 1914; it can be seen on a terrace above Manzana Creek.
The wilderness is often closed to entry during fire season, the exact dates of which vary but usually include the late summer and early fall. Most of the wilderness was burned in the 1966 Wellman Fire, and during July, August, and September 2007, the western, southern, and eastern parts of the wilderness are burned for the first time in 41 years (for the western portion) and for more than 100 years (for the remainder), in the
Zaca Fire.
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At its creation in 1968 the San Rafael Wilderness consisted of only . In 1992, after the passage of the Los Padres Condor Range and River Protection Act, Congress added an additional adjacent to the original area on the northwest. The wilderness is also adjacent to the
Dick Smith Wilderness to the east; this protected area was created in 1984.
Further Information
Get more info on 'San Rafael Wilderness'.
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