Los Angeles Basin

The Los Angeles Basin is the coastal sediment-filled plain located between the peninsular and transverse ranges in southern California in the United States containing the central part of the city of Los Angeles as well as its southern and southeastern suburbs (both in Los Angeles and Orange counties). It is approximately 35 mi (56 km) long and 15 mi (24 km) wide, bounded by the Santa Monica Mountains, the Verdugo Mountains, and the Santa Ana Mountains. The Palos Verdes Peninsula, formerly an island, marks the outer edge of the basin along the coast.

Related Topics:
Sediment - Peninsular - Transverse ranges - California - United States - Los Angeles - Los Angeles - Orange - Santa Monica Mountains - Verdugo Mountains - Santa Ana Mountains - Palos Verdes Peninsula

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The sediment in the basin is up to 6 mi (10 km) deep. The basin began to form during the Neogene approximately 15 million years ago (mya), when the terrain was underwater, during a crustal upheaval caused by a clockwise shift in the surrounding mountains. The underlying crustal weakening resulted in the formation of the large bowl of the basin. Sediment from the sea and rivers accumulated in the undersea bowl, building up in thick layers. The accumulation of micro-organisms during this time is believed to the source of the large deposits of petroleum, including the large Wilmington Oil Field, that were once under the basin but have been largely extracted. Approximately 5 million years ago, the crustal stretching subsided and the ocean floor of the basin was forced to the surface. Additional sedimental accumulated during the upswell resulting in the floor of the basin as it exists today.

Related Topics:
Neogene - Mya - Micro-organism - Petroleum - Wilmington Oil Field

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The sedimentary character of the basin is the principal reason why it is considered especially susceptible to excessive damage during earthquakes. The basin is often compared by geologists to a "a bowl of jelly" that can shake violently when driven by seismic activity. Its loose rock structure has also led to numerous instances of subsidence as a result of petroleum extraction, the most spectacular examples being the Baldwin Hills dam collapse of 1963 and the sinking of the bed of Long Beach Harbor by several meters.

Related Topics:
Earthquake - Geologist - Seismic - Baldwin Hills - Long Beach

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