1963 Kuril Islands earthquake

1963 Kuril Islands earthquake
October 13
October 20
UTC time1963-10-13 05:17:59
ISC event873239
USGS-ANSSComCat
Local dateOctober 13, 1963 (1963-10-13)
Local time15:17:59
Duration93 seconds
Magnitude8.5 Mw
Depth47 km (29.2 mi)
Epicenter44°49′N 149°32′E / 44.81°N 149.54°E / 44.81; 149.54
Areas affectedSoviet Union
Max. intensityMMI IX (Violent)[1]
TsunamiYes

The 1963 Kuril Islands earthquake occurred at 05:17 UTC, on October 13.[2] The earthquake had a magnitude of 8.5 and was followed by a Mw 7.8 event seven days later.[3] Both earthquakes triggered tsunamis that were observed around the northern part of the Pacific Ocean.

Tectonic setting

The Kuril Islands form part of the island arc formed above the subduction zone, where the Pacific plate is being subducted beneath the North American plate. This convergent boundary has been the site of many large megathrust earthquakes, including the second largest earthquake ever recorded.

Damage

No damage, deaths, or injuries were recorded for these two earthquakes or their associated tsunamis.

Characteristics

Earthquake

The megathrust earthquake ruptured a 250 km-long section of the Kuril–Kamchatka Trench which based on pulses of shock registered on seismometer records, found to have contained three particular areas of asperity with high amounts of slip inside the torn subduction interface, each roughly 50 km in length and Mw 7.5 in energy.[4]

Tsunami

The tsunami triggered by the earthquake of October 13, caused a 4.5 m wave locally. The tsunami was also observed in Canada, Japan, Mexico, Hawaii, Alaska, California, and on many islands across the northern Pacific Ocean. The tsunami associated with the October 20 event was larger in the nearby area, with a maximum recorded run-up of 15 m at Urup, but was only observed in the western part of the northern Pacific.[1]

See also

References

  1. ^ a b NGDC. "Search results page showing the two events". Archived from the original on December 14, 2012. Retrieved 12 March 2010.
  2. ^ "M5.3 – Kuril Islands (BETA)" U.S. Geological Survey. Retrieved 2014-9-4.
  3. ^ "Rupture process of the Great 1963 Kurile Islands Earthquake Sequence: Asperity interaction and multiple event rupture" SAO/NASA Astrophysics Data System. Retrieved 2014-9-5.
  4. ^ Ruff, L.; Kanamori H. (1983). "Seismic coupling and uncoupling at subduction zones" (PDF). Tectonophysics. 99 (2–4): 99–117. Bibcode:1983Tectp..99...99R. doi:10.1016/0040-1951(83)90097-5. Archived from the original (PDF) on 2010-07-23. Retrieved 2010-03-12.