Tsunami hazards to U.S. coasts from giant earthquakes in Alaska

Abstract

In the aftermath of Japan's devastating 11 March 2011 M w 9.0 Tohoku earthquake and tsunami, scientists are considering whether and how a similar tsunami could be generated along the Alaskan‐Aleutian subduction zone (AASZ). A tsunami triggered by an earthquake along the AASZ would cross the Pacific Ocean and cause extensive damage along highly populated U.S. coasts, with ports being particularly vulnerable. For example, a tsunami in 1946 generated by a M w 8.6 earthquake near Unimak Pass, Alaska (Figure 1a), caused signifcant damage along the U.S. West Coast, took 150 lives in Hawaii, and inundated shorelines of South Pacific islands and Antarctica [ Fryer et al. , 2004; Lopez and Okal , 2006]. The 1946 tsunami occurred before modern broadband seismometers were in place, and the mechanisms that created it remain poorly understood.