hazard identification and vulnerability analysis - Mason County
hazard identification and vulnerability analysis - Mason County
hazard identification and vulnerability analysis - Mason County
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Deep Earthquakes: The three most recent damaging earthquakes in<br />
Washington, in 2001 (magnitude 6.8, near Olympia), 1965 (magnitude 6.5,<br />
located between Seattle <strong>and</strong> Tacoma), <strong>and</strong> in 1949 (magnitude 7.1, near<br />
Olympia), were roughly 40 miles deep <strong>and</strong> were in the oceanic plate where it lies<br />
beneath the continent. Each earthquake caused serious damage, <strong>and</strong> was felt as<br />
far away as Montana. No aftershocks were felt following the 1965 <strong>and</strong> 1949<br />
earthquakes, <strong>and</strong> only 2 small aftershocks were felt after the 2001 quake. Other<br />
sizable events which were probably deep occurred in 1882, 1909, <strong>and</strong> 1939.<br />
Shallow Crustal Earthquakes: The largest historic earthquake in Washington or<br />
Oregon occurred in 1872 in the North Cascades. This earthquake had an<br />
estimated magnitude of 7.4 <strong>and</strong> was followed by many aftershocks. It was<br />
probably at a depth of 10 miles or less within the continental crust. Many other<br />
crustal sources in Washington <strong>and</strong> Oregon could also produce damaging<br />
earthquakes. Recent studies have found geologic evidence for large shallow<br />
earthquakes 1,100 years ago within the central Puget Basin. Massive block<br />
l<strong>and</strong>slides into Lake Washington, marsh subsidence <strong>and</strong> tsunami deposits at<br />
West Point in Seattle, tsunami deposits at Cultus Bay on Whidbey Isl<strong>and</strong>, <strong>and</strong><br />
large rock avalanches on the southeastern Olympic Peninsula have all been<br />
dated to approximately 1,100 years ago.<br />
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