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Small tar pit. La Brea Tar Pits is an active paleontological research site in urban Los Angeles. Hancock Park was formed around a group of tar pits where natural asphalt (also called asphaltum, bitumen, or pitch; brea in Spanish) has seeped up from the ground for tens of thousands of years.
On June 29, 1952, the McKittrick Tar Pits were registered a California Historical Landmark. California Historical Landmark reads: NO. 498 McKITTRICK BREA PIT - Located one-eighth mile west of here is an ancient asphaltum seepage in which hundreds of Pleistocene Age (15,000-50,000 years ago) birds and animals were trapped.
Badger fossils make up approximately 0.39% of the total carnivoran fauna at Rancho La Brea. It is possible that some of the badgers may have become trapped when tar entered their burrows. American black bear [22] [23] Ursus americanus: Among the black bear remains from La Brea is the skull of a juvenile individual.
Older fossils lay even deeper beneath the bone bed. These 8.9-million-year-old rocks included fossilized bones of fish and marine mammals. Experts also found teeth from juvenile megalodons and ...
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The Marble Mountains Fossil Beds are the site of 550-million-year-old fossils of trilobites, which were among the first animals on earth with eyes and skeletons. In all, roughly 21 species of Cambrian invertebrates have been discovered in the area. [ 4 ]
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 Capistrano Formation, named for the town of San Juan Capistrano, is located in southern California, specifically the northern extent of the Peninsular Ranges, which stretch from the Los Angeles Basin to Baja California. [2] It crops out along the coast from Dana Point to San Clemente, and inland for seven miles. [1]