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Bulletin of the Seismological Society of America; December 2002; v. 92; no. 8; p. 3239-3258; DOI: 10.1785/0120010274
© 2002 Seismological Society of America
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Article

The December 1872 Washington State Earthquake

William H. Bakun, Ralph A. Haugerud, Margaret G. Hopper and Ruth S. Ludwin

U.S. Geological Survey
345 Middlefield Rd MS977
Menlo Park, California 94025
(W.H.B.)
U.S. Geological Survey
University of Washington
Box 351310, Seattle, Washington 98195
(R.A.H.)
U.S. Geological Survey
P.O. Box 25046
Lakewood, Colorado 80225
(M.G.H.)
Dept. of Earth and Space Sciences
University of Washington
Box 351310, Seattle, Washington 98195
(R.S.L.)

Manuscript received 23 October 2001.

The largest historical earthquake in eastern Washington occurred on 15 December 1872. We used Modified Mercalli intensity (MMI) assignments for 12 twentieth-century earthquakes to determine attenuation relations for different regions in the Pacific Northwest. MMI attenuation for propagation paths east and west of the Cascade Mountains differs significantly only for epicentral distances greater than about 225 km. We used these attenuation relations and the MMI assignments for the 15 December 1872 earthquake to conclude that its epicentral region was east of the Cascade Mountains near Lake Chelan, Washington, and most probably near the south end of Lake Chelan. The intensity magnitude, MI, is 6.8 and moment magnitude, M, is 6.5-7.0 at the 95% confidence level.




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