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Agenda - City of Santa Monica

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THREAT ASSESSMENT 1 – MAJOR EARTHQUAKE<br />

General Situation<br />

Since 1800 there have been approximately 60 damaging seismic events, or<br />

"earthquakes," in the Los Angeles region. After a brief hiatus between major events<br />

(circa 1940-1972), the greater Los Angeles area has experienced a number <strong>of</strong><br />

moderate events which have resulted in considerable disruption <strong>of</strong> the infrastructure,<br />

impact on social and economic life, loss <strong>of</strong> lives and extensive property damage within<br />

the <strong>City</strong> <strong>of</strong> Los Angeles, the greater metropolitan area and the adjacent region including<br />

<strong>Santa</strong> <strong>Monica</strong>. According to the Geological Survey's records, some 20 quakes <strong>of</strong><br />

magnitude 6.0 or higher have occurred in Southern California since 1912. The most<br />

recent <strong>of</strong> these was the M6.7, 1994 Northridge Earthquake which was centered in the<br />

northwest part <strong>of</strong> the <strong>City</strong>, in the general vicinity <strong>of</strong> the 1971 San Fernando (a.k.a.<br />

Sylmar) quake.<br />

Following the 1994 Northridge and 1995 Kobe, Japan earthquakes, a variety <strong>of</strong> studies<br />

and cooperative information exchange ventures were initiated to expand knowledge<br />

concerning earthquakes so that people could be better protected in the event <strong>of</strong> future<br />

significant seismic events. Kobe, Northridge and other seismic event information are<br />

being used in formulating methodologies for strengthening buildings and structures to<br />

more successfully withstand severe damage and to better protect occupants and<br />

equipment during various types and degrees <strong>of</strong> seismic events.<br />

The California State Geologist's Seismic Hazards Mapping Program has provided maps<br />

that identify amplified shaking, liquefaction and landslide hazard zones. These maps are<br />

used in revising the <strong>City</strong>’s building, zoning and other codes, plans, standards,<br />

procedures and/or development permit requirements.<br />

Based on Richter scale and pre-Richter calculations, the second most-powerful tremor<br />

recorded in Los Angeles proper was in 1923 and centered in the San Jacinto<br />

Mountains, southeast <strong>of</strong> the <strong>City</strong>. The M6.3 earthquake caused only light damage in Los<br />

Angeles. In 1918, also in the isolated San Jacinto Mountains, some 150 miles from<br />

downtown, a mighty M6.8 quake occurred.<br />

Los Angeles experienced two quakes <strong>of</strong> identical 6.3 magnitude - one in the Long<br />

Beach area in 1933 and another in <strong>Santa</strong> Barbara in 1925—that produced disastrous<br />

damage because their epicenters were near central cities. The Long Beach toll was $40<br />

million in property destruction and 115 lives lost. The <strong>Santa</strong> Barbara shake leveled<br />

much <strong>of</strong> the business district at a $6 million loss there, and killing 20.<br />

An earthquake in 1927 ranks--along with Tehachapi-Bakersfield in 1952--as the all-time<br />

southern California strongest earthquakes. Registering at M7.5, the 1927 upheaval<br />

centered just north <strong>of</strong> Point Arguello in the upper <strong>Santa</strong> Barbara channel, destroying<br />

railways bridges, crumbling cliffs and sending a seismic wave as far north as Pismo<br />

255

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