The 2002 Denali Fault Earthquake, Alaska: A Large Magnitude, Slip-Partitioned Event

Donna Eberhart‐Phillips(United States Geological Survey), Peter J. Haeussler(United States Geological Survey), Jeffrey T. Freymueller(United States Geological Survey), Arthur D. Frankel(United States Geological Survey), Charles M. Rubin(United States Geological Survey), Patricia Craw(United States Geological Survey), Natalia A. Ratchkovski(United States Geological Survey), G. Anderson(United States Geological Survey), Gary A. Carver(United States Geological Survey), Anthony J. Crone(United States Geological Survey), Timothy E. Dawson(United States Geological Survey), Hilary J. Fletcher(United States Geological Survey), R. A. Hansen(United States Geological Survey), Edwin L. Harp(United States Geological Survey), Ruth Harris(United States Geological Survey), David P. Hill(United States Geological Survey), Sigrún Hreinsdóttir(United States Geological Survey), Randall W. Jibson(United States Geological Survey), Lucile M. Jones(United States Geological Survey), Robert E. Kayen(United States Geological Survey), David K. Keefer(United States Geological Survey), Christopher F. Larsen(United States Geological Survey), S. C. Moran(United States Geological Survey), Stephen F. Personius(United States Geological Survey), George Plafker(United States Geological Survey), Brian L. Sherrod(United States Geological Survey), K. Sieh(United States Geological Survey), Nicholas Sitar(United States Geological Survey), Wesley K. Wallace(United States Geological Survey)
Science
May 15, 2003
10.1126/science.1082703
Cited by 441

Abstract

The MW (moment magnitude) 7.9 Denali fault earthquake on 3 November 2002 was associated with 340 kilometers of surface rupture and was the largest strike-slip earthquake in North America in almost 150 years. It illuminates earthquake mechanics and hazards of large strike-slip faults. It began with thrusting on the previously unrecognized Susitna Glacier fault, continued with right-slip on the Denali fault, then took a right step and continued with right-slip on the Totschunda fault. There is good correlation between geologically observed and geophysically inferred moment release. The earthquake produced unusually strong distal effects in the rupture propagation direction, including triggered seismicity.

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