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Agenda - City of Santa Monica

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esponse to a seismic event. The intensity <strong>of</strong> the ground shaking and the resultant<br />

damages are determined by the magnitude <strong>of</strong> the earthquake, distance from the<br />

epicenter, and characteristics <strong>of</strong> surface geology. This hazard is the primary cause <strong>of</strong><br />

the collapse <strong>of</strong> buildings and other structures.<br />

It is generally understood that an earthquake does not in itself present a seismic hazard,<br />

but that it becomes a hazard when it occurs in a highly urbanized area. Therefore, the<br />

significance <strong>of</strong> an earthquake's ground shaking action is directly related to the density<br />

and type <strong>of</strong> buildings and number <strong>of</strong> people exposed to its effect.<br />

Earthquake Induced Landslides<br />

Earthquake induced landslides are secondary earthquake hazards that occur from<br />

ground shaking. They can destroy the roads, buildings, utilities, and other critical<br />

facilities necessary to respond and recover from an earthquake. The <strong>City</strong> <strong>of</strong> <strong>Santa</strong><br />

<strong>Monica</strong> has a high likelihood <strong>of</strong> encountering such risks, especially in areas with steep<br />

slopes.<br />

Liquefaction<br />

Liquefaction <strong>of</strong> soil may occur in the beach area. Structures, including the <strong>Santa</strong><br />

<strong>Monica</strong> Pier, which are otherwise sound, may collapse if built on sandy water-saturated<br />

ground. Liquefaction is a phenomenon involving the loss <strong>of</strong> shear strength <strong>of</strong> a soil. The<br />

shear strength loss results from the increase <strong>of</strong> poor water pressure caused by the<br />

rearrangement <strong>of</strong> soil particles induced by shaking or vibration. Liquefaction has been<br />

observed in many earthquakes, usually in s<strong>of</strong>t, poorly graded granular materials (i.e.,<br />

loose sands), with high water tables. Liquefaction usually occurs in the soil during or<br />

shortly after a large earthquake. In effect, the liquefaction soil strata behave as a heavy<br />

fluid. Buried tanks may float to the surface and objects above the liquefaction strata<br />

may sink. Pipelines passing through liquefaction materials typically sustain a relatively<br />

large number <strong>of</strong> breaks in an earthquake.<br />

Damage to Vital Public Services, Systems and Facilities<br />

Bed Loss in Hospitals<br />

<strong>Santa</strong> <strong>Monica</strong> has two major hospitals with a total capacity <strong>of</strong> 532 beds. Public service<br />

agencies and volunteer personnel would be used to assist in the care <strong>of</strong> the injured.<br />

<strong>Santa</strong> <strong>Monica</strong> UCLA<br />

The <strong>Santa</strong> <strong>Monica</strong>-UCLA Medical Center is staffed by more than 900 employees,<br />

whose efforts are complemented by over 300 volunteers and 200 care extenders. The<br />

medical staff consists <strong>of</strong> 750 physicians representing virtually all medical and surgical<br />

specialties.<br />

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