| Geology-208 | 
Types of earthquakes are:
Deep quakes (subducting slabs)  least destructive
The Seattle-area earthquake this year (2001) was centered 30 miles beneath the earth's surface, underneath Anderson Island, east of Olympia. All our strongly-felt earthquakes have "occurred as one plate of the earth's crust slowly slid farther beneath another." (Christian Science Monitor, March 2, 2001).
Shallow faults  more destructive
Plate boundary quakes  catastrophic
| Divergent boundaries: adjacent plates move away from each other | 
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| Convergent boundaries: adjacent plates move toward each other | 
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| Transform boundaries: adjacent plates slide side by side past each other | 
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| Hot spot: intraplate; volcanism and quakes are caused by the continental plate passing over a “hot spot” in the earth’s mantle | 
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Send comments to Rob Viens (e-mail: rviens@bcc.ctc.edu) or call him at his Bellevue Community College office at (425) 564-3158. Office hours are by appointment.