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A possible source mechanism of the 1946 Unimak Alaska far-field tsunami, uplift of the mid-slope terrace above a splay fault zone

Roland E. von Huene·John J. Miller·Dirk Klaeschen·Peter Dartnell
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Abstract

In 1946, megathrust seismicity along the Unimak segment of the Alaska subduction zone generated the largest ever recorded Alaska/Aleutian tsunami. The tsunami severely damaged Pacific islands and coastal areas from Alaska to Antarctica. It is the charter member of “tsunami” earthquakes that produce outsized far-field tsunamis for the recorded magnitude. Its source mechanisms were unconstrained by observations because geophysical data for the Unimak segment were sparse and of low resolution. Reprocessing of legacy geophysical data reveals a deep water, high-angle reverse or splay thrust fault zone that leads megathrust slip upward to the mid-slope terrace seafloor rather than along the plate boundary toward the trench axis. Splay fault uplift elevates the outer mid-slope terrace and its inner area subsides. Multibeam bathymetry along the splay fault zone shows recent but undated seafloor disruption. The structural configuration of the nearby Semidi segment is similar to that of the Unimak segment, portending generation of a future large tsunami directed toward the US West coast.

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Pure and Applied GeophysicsArticle
90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 52° to 58° latitude; -168° to -154° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Roland E. von Huene, John J. Miller, Dirk Klaeschen, Peter Dartnell. 2016-09-22. A possible source mechanism of the 1946 Unimak Alaska far-field tsunami, uplift of the mid-slope terrace above a splay fault zone. https://doi.org/10.1007/s00024-016-1393-x

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