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Anza is a census-designated place located in southwestern Riverside County, California, in the Anza Valley, a semi-arid region at a mean elevation of 3,921 feet (1,195 m) above sea level. It is located 13 miles (21 km) south of Idyllwild , [ 3 ] 32 miles (51 km) east-northeast of Temecula , 40 miles (64 km) southwest of Palm Springs , and 90 ...
Anza Valley, formerly known as the Hamilton Plains, [1] is a basin in Riverside County, California. It lies at an elevation of 4,157 feet (1,267 m), west of the San Jacinto and Santa Rosa Mountains .
Coyote Creek is the only reliably perennial creek in Anza-Borrego Desert State Park. Coyote Creek is 18 miles (29 km) long and runs from the city of Anza, California to Borrego Sink. Borrego Sink is at an elevation of 455 feet (138 meters) at the low spot of the Borrego Valley.
California: Foothill–De Anza Community College: 89.7 FM ... California: California State University, Stanislaus ... Illinois: Illinois State University: 103.3 FM
The region consists predominantly of Anza Borrego Desert State Park, the largest state park in California. and occupies all of San Diego County east of the Peninsular Ranges with the exception of the Mountain Empire. Central, or Central San Diego, includes most of the city of San Diego, often together with Coronado, excluding South San Diego ...
Anza-Borrego Desert State Park (/ ˈ æ n z ə b ə ˈ r eɪ ɡ oʊ /, AN-zə bə-RAY-goh) is a California State Park located within the Colorado Desert of Southern California, United States. The park takes its name from 18th century Spanish explorer Juan Bautista de Anza and borrego , a Spanish word for sheep. [ 1 ]
The Ramona Indian Reservation was founded in 1893. It is about 560 acres (2.3 km 2) large, located in Anza, California at the foot of Thomas Mountain.The land was originally Sauppalpisa territory and was a traditional gathering place for Cahuilla ceremonies.
The Mud Caves are a popular feature in Anza Borrego Desert State Park in San Diego County, California.The caves, located in the Carrizo Badlands, along the Arroyo Tapiado, were created by water flowing through a thick deposit of silt and are an example of pseudokarst topography.