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Lecture 6: Tsunamis Our Hazardous Environment GEOG 1110 Dr. Thieme
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Tsunami Japanese for "large harbor wave" catastrophic impacts occur thousands of kilometers from geologic source Four possible causes –earthquake (along subduction zone) –underwater landslide –collapse of a volcano –asteroid impact
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Subduction Zone
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Indonesian Tsunami Indian and Australian plates eastward subduction beneath Eurasian plate "stick-slip" of subducting plates M 9.1 Earthquake on December 26, 2004
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Banda Aceh provincial capital on northern Sumatra shaking by earthquake pummeling waves flooding after land subsided
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Distant vs. Local water depth varies as wave departs epicenter wave splits into "local" tsunami along adjacent coast "distant" tsunami in deep water
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Local Tsunami 1993 in Sea of Japan 15-30 m waves struck Okushiri Island arrived only 2-5 minutes after earthquake 120 people killed
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Tsunami Warning System "buoys in the ocean" depth gauges water pressure recorder on sea bottom also need PUBLIC EDUCATION ! !
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Tsunami Runup Map
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Tsunami Hazard Map indicates possible areas of wave impact based upon elevation slope of sea bottom orientation of coast
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