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Constraints on the Slip Distribution of the 1938 M W 8.3 Alaska Peninsula Earthquake From Tsunami Modeling

2021; American Geophysical Union; Volume: 48; Issue: 9 Linguagem: Inglês

10.1029/2021gl092812

1944-8007

J. T. Freymueller, E. N. Suleimani, Dmitry Nicolsky,

High-pressure geophysics and materials

Abstract We simulated tsunami propagation for several scenario slip distributions for the 1938 M W 8.3 earthquake along the Alaska Peninsula and compared these to the observed records at Unalaska/Dutch Harbor and Sitka. The Sitka record is sensitive to the depth of slip but not the along‐strike location and is fit best by slip at shallow depth. The Unalaska record is sensitive mainly to the along‐strike location of slip and is fit best by slip that is concentrated in the eastern part of the presumed 1938 rupture zone. The tsunami data show that the actual 1938 earthquake rupture zone was likely ∼200 km in length or shorter and had no slip near the Shumagin Islands or in the 2020 Simeonof earthquake's rupture zone. The rupture models that best predict the 1938 tsunami lie within the region of high present day slip deficit inferred from GPS.