Roland E. von Huene Dave Scholl Stephen Kirby Holly F. Ryan 2012 In the aftermath of Japan's devastating 11 March 2011M_<i>w</i> 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 <i>M_w</i> 8.6 earthquake near Unimak Pass, Alaska (Figure 1a), caused significant damage along the U.S. West Coast, took 150 lives in Hawaii, and inundated shorelines of South Pacific islands and Antarctica [<i>Fryer et al.</i>, 2004; <i>Lopez and Okal</i>, 2006]. The 1946 tsunami occurred before modern broadband seismometers were in place, and the mechanisms that created it remain poorly understood. application/pdf 10.1029/2012EO190001 en American Geophysical Union Tsunami hazards to U.S. coasts from giant earthquakes in Alaska article