1965 Rat Islands earthquake

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1965 Rat Islands earthquake
Relief map of USA Alaska.png
Bullseye1.png
UTC  time1965-02-04 05:01:22
ISC  event 859206
USGS-ANSS ComCat
Local dateFebruary 3, 1965 (1965-02-03)
Local time19:01:22
Magnitude8.7 Mw
Depth30.3 km (19 mi)
Epicenter 51°17′N178°33′E / 51.29°N 178.55°E / 51.29; 178.55
Areas affectedUnited States (Alaska)
Total damage$10,000
Max. intensity MMI VI (Strong) [1]
Tsunami10.7 m (35 ft)

The 1965 Rat Islands earthquake occurred at 05:01 UTC, on 4 February (19:01, 3 February local time [1] ). It had a magnitude of 8.7 and triggered a tsunami of over 10 m on Shemya Island, [2] but caused very little damage.

Contents

Tectonic setting

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 Aleutian Trench, has been the location of many megathrust earthquakes.

Characteristics

Map showing the tectonics and seismicity of Alaska Alaska earthquakes.jpg
Map showing the tectonics and seismicity of Alaska

The 1965 Rat Islands earthquake share common features with the 1963 Kuril Islands earthquake and the 1964 Alaska earthquake. [3]

Earthquake

The earthquake was associated with a 600 km long rupture along the plate boundary, based on the distribution of aftershocks. [4] 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. [5]

The main shock was followed by an earthquake of magnitude 7.6 nearly two months later, that triggered a small tsunami. [1] This was not an aftershock, but a normal fault event within the outer rise of the subducting plate, triggered by the earlier event. [6]

Tsunami

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. [1]

Damage

Flooding from the tsunami caused $10,000 worth of damage on Amchitka Island. [2] Minor damage from the earthquake was recorded on both Attu and Shemya islands in the form of cracks in runways.

See also

Related Research Articles

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The 1979 Yapen earthquake occurred on September 12 at 05:17:51 UTC. It had an epicenter near the coast of Yapen Island in Irian Jaya, Indonesia. Measuring 7.5 on the moment magnitude scale and having a depth of 20 km (12 mi), it caused severe damage on the island. At least 115 were killed due to shaking and a moderate tsunami.

The 1979 Saint Elias earthquake affected Alaska at 12:27 AKST on 28 February. The thrust-faulting Mw 7.5 earthquake had an epicenter in the Granite Mountains. Though the maximum recorded Modified Mercalli intensity was VII, damage was minimal and there were no casualties due to the remoteness of the faulting. Damage also extended across the border in parts of Yukon, Canada.

The 1958 Kuril Islands earthquake or Etorofu earthquake was a Mw 8.3–8.4 earthquake that struck near the Kuril island of Iturup on November 6, 1958, at 22:58 UTC, or 09:58 on the 7th local time. The earthquake occurred as the result of shallow reverse faulting along the Kuril-Kamchatka Trench, and caused Modified Mercalli Intensity (MMI) X (Extreme) shaking, as well as a tsunami 5 m (16 ft) high. Iturup sustained significant damage as a result of the shaking and tsunami, with other locations along the Kuril Islands also reporting strong damage.

References

  1. 1 2 3 4 NGDC. "Search result for 1965 Alaska earthquakes". Archived from the original on December 30, 2017. Retrieved 8 March 2010.
  2. 1 2 "Historic Earthquakes Rat Islands, Alaska". United States Geological Survey. 26 October 2009. Archived from the original on 16 January 2010. Retrieved 8 March 2010.
  3. Wu, Francis T.; Kanamori, Hiroo (9 October 1973). "Source mechanism of February 4, 1965, Rat Island earthquake". Journal of Geophysical Research. 78 (26): 6082–6092. Bibcode:1973JGR....78.6082W. doi:10.1029/jb078i026p06082.
  4. Beck, Susan L.; Christensen, Douglas H. (1991). "Rupture process of the February 4, 1965, Rat Islands Earthquake". Journal of Geophysical Research. 96 (B2): 2205. Bibcode:1991JGR....96.2205B. doi:10.1029/90JB02092.
  5. Johnson, Jean M. (1998). "Heterogeneous Coupling Along Alaska-Aleutians as Inferred from Tsunami, Seismic, and Geodetic Inversions". Tsunamigenic Earthquakes and Their Consequences. Advances in Geophysics. Vol. 39. pp. 1–116. doi:10.1016/S0065-2687(08)60275-7. ISBN   978-0-12-018839-0.
  6. Abe, Katsuyuki (January 1972). "Lithospheric normal faulting beneath the Aleutian trench". Physics of the Earth and Planetary Interiors. 5: 190–198. Bibcode:1972PEPI....5..190A. doi:10.1016/0031-9201(72)90091-X.

Further reading