1965 Rat Islands earthquake
|Date||February 4, 1965|
|Areas affected||United States (Alaska)|
The Rat Islands form part of the Aleutian Islands, a chain of volcanic islands forming an island arc, that results from the subduction of the Pacific Plate beneath the North American Plate. This plate boundary, the Alaska-Aleutian megathrust, has been the location of many megathrust earthquakes.
The earthquake was associated with a 600 km long rupture along the plate boundary, based on the distribution of aftershocks. The pattern of energy release suggest the presence of three asperities along the plate interface, each causing a pulse of moment release. Modelling of the tsunami supports the idea that the earthquake consisted of three sub-events, related to three structural 'blocks' within the overriding plate.
The main shock was followed by an earthquake of magnitude 7.6 nearly two months later, that triggered a small tsunami. This was not an aftershock, but a normal fault event within the outer rise of the subducting plate, triggered by the earlier event.
The tsunami had a maximum run-up height of 10.7 m on Shemya Island, 2.0 m at Amchitka Island, 1.6 m at Attu Island and 1.1 m in northern Kauai, Hawaii. It was also observed in Peru, Ecuador, Mexico, California, Japan and eastern Russia.
- USGS (26 October 2009). "Historic Earthquakes Rat Islands, Alaska". Retrieved 8 March 2010.
- Beck, S.L.; Christensen D.H. (1991). "Rupture Process of the February 4, 1965, Rat Islands Earthquake". Journal of Geophysical Research 96 (B"): 2205–2221. Bibcode:1991JGR....96.2205B. doi:10.1029/90JB02092. Retrieved 2010-03-08.
- Johnson, J.M. (1999). "Heterogeneous coupling along Alaska-Aleutians as inferred from Tsunami, Seismic and Geodetic Inversions". In Dmowska R. & Saltzman B. Tsunamigenic Earthquakes and Their Consequences. Advances in Geophysics 39. pp. 28–55. ISBN 978-0-12-018839-0. Retrieved 2010-03-08.
- NGDC. "Search result for 1965 Alaska earthquakes". Retrieved 8 March 2010.
- Abe, K. (1972). "Lithospheric normal faulting beneath the Aleutian trench". Physics of the Earth and Planetary Interiors 5: 109–198. Bibcode:1972PEPI....5..190A. doi:10.1016/0031-9201(72)90091-X.