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- W2123494147 abstract "On November 03, 2002, a magnitude 7.9 earthquake shook the interior of Alaska. This is the largest known event on the Denali Fault system. It was preceded by the M6.7 Nenana Mountain earthquake on October 23, 2002, which was located 44 km northeast of the Denali National Park entrance and 146 km south of Fairbanks. The Nenana Mountain earthquake ruptured 45 km of the Denali Fault. The Denali Fault earthquake initially occurred within the Nenana Mountain earthquake rupture zone, on the Susitna Glacier thrust fault. The earthquake propagated along the Susitna Glacier fault to the adjoining Denali strike-slip fault. The propagation continued eastward along the Denali fault until it reached the junction between the Denali and Totschunda faults, where the rupture transferred to the southeast trending Totschunda strike-slip fault. The rupture occurred over 345 km on three different faults with three distinct releases of concentrated energy in a time span of 1.5 to 2 minutes. Since the rupture propagated east, the majority of the energy released by the earthquake also propagated east, away from Fairbanks and Anchorage. This resulted in minimal damages in the two main population centers of Alaska. The most damage was in the town of Mentasta Lake, where on the nearby Tok Highway cutoff, the maximum fault offsets of 8.8 m were located." @default.
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- W2123494147 date "2003-01-01" @default.
- W2123494147 modified "2023-09-27" @default.
- W2123494147 title "Moment tensors and focal mechanisms of the October-November Denali Fault earthquake sequence - Abstract" @default.
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