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Plate Tectonic

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Plate Tectonics Paper Name: Tonia Erskine Date: 01/09/2015 Instructor: Allen Fronabarger

According to the U.S. Geological Survey (USGS) one of the leading agency that monitor real time earthquake in the state of Los Angeles, states it is a very high risk for frequent damaging earthquakes. These earthquakes are results from many fault systems that moving through Los Angeles that leads to earthquakes of many different types and sizes. South California has more than 10,000 earthquakes every year; many of them are very small and sometime never even cause any damage or even felt. However, Los Angeles do have large earthquake that create after shocks the causes many damages and sometimes these aftershock can create sequence of additional earthquake that can occur for months. On March 10, 1933 at 5:54 p.m. magnitude 6.4 earthquakes hit the Newport-Inglewood Fault, causing serious damage in Long Beach and other communities. The earthquake resulted in 120 deaths and more than $50 million in property damage. Most of the damaged buildings were of unreinforced masonry. The most recent earthquake in South California caused severe structural damage to buildings but did not caused any deaths, however, on February 9, 1971 caused the city about $500 million in damages and 65 deaths. On October 1, 1987 at 7:42 a.m. an earthquake of the magnitude 5.9. struck the city causing eight deaths and $358 million property damages.

Earthquake is caused when the two sided of a fault slip suddenly against each other. The frictions between the plates will cause stress this then in turn will release blocks of crust that will eventually slip suddenly along a fault plane. When this occurs it then releases waves of energy that is commonly known as shockwaves, which moves through the

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