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Faults and Earthquakes. Some faults become “locked” –Pressure pushes together the irregular walls of the fault; surfaces resist sliding Slip can’t occur.

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Presentation on theme: "Faults and Earthquakes. Some faults become “locked” –Pressure pushes together the irregular walls of the fault; surfaces resist sliding Slip can’t occur."— Presentation transcript:

1 Faults and Earthquakes

2 Some faults become “locked” –Pressure pushes together the irregular walls of the fault; surfaces resist sliding Slip can’t occur until enough stress is built up to overcome resistance

3 Earthquake ! Focus - point of initial rupture Epicenter - point on surface directly above the focus

4 The energy released by the earthquake increases with (a) the area of the fault plane that slips (b) the slip distance (c) the strength of the rocks It’s easy to break contact points on a small section of fault, that allows a little slip. Large slip on big sections of a fault, requires an rare alignment of contacts points. therefore larger earthquakes are rarer than small earthquakes.

5 Earthquake Damage - ground displacement

6 Earthquake Damage - shaking

7 San Francisco, 1906 Earthquake Damage - fire

8 Measurement of Earthquake Magnitude, continued –M 5 earthquake versus M 7 earthquake M 7 has 100X stronger shaking, ~900X the energy Magnitude is measured on a Logarithmic Scale An increase in 1 whole number represents an earthquake that has 10 times stronger ground motion ~30 times as much energy release

9 Sources of Earthquake Damage shaking liquifaction- shaking can cause water-saturated soil to behave like a fluid: buildings sink or tip over fire tsunami landslides ground displacement

10 Dangerous factors contributing to earthquake deaths Dense populations Building style Time of day Relief infrastructure

11 Earthquake Hazard

12 California Earthquakes 1989 Loma Prieta -6.9 1999 Hector Mine 7.1 1992 Landers 7.3 1994 Northridge 6.9 1972 San Fernando 6.6 1933 Long Beach 6.4 1952 Kern County 7.3 1872 Owens Valley 7.6 1857 Fort Tejon 7.9 1983 Coalinga 6.7 1906 San Francisco 7.9

13 Tsunami (incorrectly called “tidal wave”) Open sea Wave height: cm to 1 m Speed: 750 km/hr Near shore Wave height: up to tens of meters Seismically-induced sea wave

14 2004 Indian Ocean Tsunami

15 2004 Sumatra “Tsunami” Earthquake Dec. 26, 2004 : M 9.0 earthquake (4th largest recorded) occurs off northern Sumatra; ~500 km section of fault moves, with max. of 20 m of slip

16 Several meters of seafloor movement triggers tsunami Wave height on Sumatra - 30 m Thailand - 10 m Sri Lanka - 15 m India - 5 m


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