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  2. Anza-Borrego Desert State Park - Wikipedia

    en.wikipedia.org/wiki/Anza-Borrego_Desert_State_Park

    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 ]

  3. Borrego Sink - Wikipedia

    en.wikipedia.org/wiki/Borrego_Sink

    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. Coyote Creek supports Desert bighorn sheep and a desert riparian ...

  4. Galleta Meadows Estate - Wikipedia

    en.wikipedia.org/wiki/Galleta_Meadows_Estate

    Borrego Springs is a village completely surrounded by Anza-Borrego Desert State Park, the largest state park in California. The Galleta Meadows metal sculptures have different themes. [5] The largest theme appears to be of prehistoric animals, including dinosaurs.

  5. Anza-Borrego Desert State Park: Located between San Diego and the Salton Sea, Anza-Borrego is the largest state park in California. "Visitors can see remaining sand verbena and desert sunflowers ...

  6. Yaqui Well - Wikipedia

    en.wikipedia.org/wiki/Yaqui_Well

    Yaqui Well is a historic spring located in Anza-Borrego Desert State Park in southeastern San Diego County, California in the United States about 21.4 mi (34.4 km) east of Warner Springs. [2] The watering hole can be reached by a popular 1.64 mi (2.64 km) one-hour (round trip) hiking trail starting at Tamarisk Grove Campground. [3]

  7. Mud Caves - Wikipedia

    en.wikipedia.org/wiki/Mud_Caves

    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.