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Asphalt Deposits

Millions of years ago, the area of Los Angeles and Rancho La Brea lay beneath the surface of the Pacific Ocean. During this time, marine sedimentary layers formed and in some places these eventually became rich with fossil fuels produced from ancient sea life. When the ocean levels receded some 100,000 years ago, the area of Rancho La Brea became land. New layers of gravel, sand, and clay formed by the erosion of the emergent hills, and settled on top of the much older marine sediments full of oil.

At Rancho La Brea, the crude oil has been seeping out of the ground through conduits and fissures in the coastal plain sediments for the past 40,000 years, the seeps forming pools in low-lying areas.

Asphalt Deposits

Foot Note!
Commonly called the "tar pits," the liquids that seep out of the ground at Rancho La Brea are actually comprised of asphalt, not tar. Tar is a commercial by-product made by the distillation of woody materials, such as coal or peat, while asphalt is a naturally formed substance comprised of hydrocarbon molecules.
 


Asphalt Deposits
Fresh sediments from the surrounding hills continued to form new layers of sediments on top of the older ones and asphalt continued to seep to the surface. Over tens of thousands of years, this produced the cone-shaped asphalt deposits found at Rancho La Brea.

Foot Note!
Though asphalt seeps like those at Rancho La Brea are extremely rare, others have been found near Bakersfield, California and as far away as Peru and Iran. However, none have yielded the quantity or diversity of fossils that have been collected from Rancho La Brea.

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