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The Sonny Bono Salton Sea National Wildlife Refuge is located in the Imperial Valley of California, 40 miles (64 km) north of the Mexican border. Situated at the southern end of the Salton Sea , the refuge protects one of the most important nesting sites and stopovers along the Pacific Flyway .
It was founded in 1974 as the first urban National Wildlife Refuge established in the United States, and it is dedicated to preserving and enhancing wildlife habitat, protecting migratory birds, protecting threatened and endangered species, and providing opportunities for wildlife-oriented recreation and nature study for the surrounding communities.
The San Joaquin Marsh Wildlife Sanctuary is a 300-acre (120 ha; 0.47 sq mi) constructed wetland in Irvine, California, in the flood plain of San Diego Creek just above its outlet into the Upper Newport Bay.
Coachella Valley National Wildlife Refuge is a 3,709-acre (15.01 km 2) protected area in Riverside County, California's Coachella Valley. It lies within the unincorporated community of Thousand Palms , just north of Palm Desert .
Ex situ management can occur within or outside a species' natural geographic range. Individuals maintained ex situ exist outside an ecological niche. This means that they are not under the same selection pressures as wild populations, and they may undergo artificial selection if maintained ex situ for multiple generations. [3]
Castle Rock National Wildlife Refuge is 0.5 miles (0.80 km) offshore from Crescent City in northern California. This coastal rock covers approximately 14 acres (57,000 m 2), and rises steeply 335 feet (102 m) above sea level. The refuge provides an important sanctuary for the Aleutian cackling goose and nesting seabirds.
A Southern California city is suing the state over sanctuary laws that limit cooperation between local authorities and immigration officials. The lawsuit, which also names California Gov. Gavin ...
The refuge is located in the California Coast Ranges. Basement rocks along the coast are from the Mesozoic , 65 to are 245 million years old. About seven million years ago the local ranges experienced most of their uplift, and there are several geological faults, such as the San Gregorio-Hosgri fault system .