2017 Komandorski Islands earthquake

On July 17, an earthquake struck near the Komandorski Islands, east of the Kamchatka Peninsula in the Bering Sea at (23:34:13 UTC). Although there were no casualties from this earthquake, it was notable for a rare characteristic known as supershear, and is one of the few times a supershear earthquake has been observed. It's rupture length of 400 km is also one of the longest in the world for a strike-slip fault, comparable to the 1906 San Francisco and 2001 Kokoxili earthquake. It was preceded by a few foreshocks months earlier, and aftershocks that continued for nearly six months.[1]

2017 Komandorski Islands earthquake
UTC time2017-07-17 23:34:13
ISC event610785483
USGS-ANSSComCat
Local date
Local time
Duration> 80 seconds
Magnitude7.8 Mw
Depth10.0 km
Epicenter54.443°N 168.857°E / 54.443; 168.857
FaultBering Fracture Zone
TypeStrike-slip (Dextral)
Areas affectedRussia
Total damageNone
Max. intensityVII (Very Strong)
Tsunami0.3 ft
ForeshocksYes
AftershocksYes

Tectonic Setting

The Mww 7.7-7.8 earthquake nucleated along the Bering Fracture Zone, parallel to the Aleutian Islands arc and Aleutian Subduction Zone. This is a transform fault between the Pacific and North American Plates, and in between, the Komandorski Sliver. Formed from the highly oblique movement of the Pacific Plate, the direction of convergence is nearly parallel to the trench at 7.8 mm/yr.[2] The Bearing Fracture Zone acts as a back-arc fault to accommodate the lateral motion at a rate of 5.1 mm/yr. The same fracture zone may have produced a similar sized earthquake in 1929 close to the Near Islands of Alaska.[3] Energy released from this earthquake was sufficient to accommodate strain built-up since the last earthquake on that section of fault in 1858.[2]

Earthquake

Initially registering a magnitude 7.4, the earthquake was quickly revised to a 7.7 by the US Geological Survey.[4] No loss of life or property damage was reported following the earthquake due to the remoteness of the event, although it could be felt by people. Shaking intensities V to VI was felt at Bering Island, and in Petropavlovsk-Kamchatsky, was felt as II.[5] Tsunami warning was issued but cancelled a few less than two hours later.[6] A non-destructive tsunami of 0.3 feet was observed.[7] The small tsunami was attributed to the lack of vertical displacement during the event.

The earthquake focal mechanism was almost pure strike-slip, and the entire rupture process took more than 80 seconds.[1] Displacements of 4 to 8.5 meters along the upper 15 km of the crust, with evidence of extension at 20 to 30 km depth.[2] Evidence of supershear was discovered when researchers realized that rupture velocity of this event increased from 2.1 km/s to 5.0 km/s after the rupture jumped onto another segment at a step-over.[8] The rupture speed far exceeded the shear wave velocity.

Foreshocks and aftershocks

A magnitude 6.7 earthquake occurred close to Attu Station, Alaska on 2 June, and a 6.3 thirteen hours before the mainshock.[9][10] The 2 June foreshock had a foreshock of its own on 27 March.[11][5]

Nearly all of the aftershocks from this earthquake were relatively small, mostly in the M4.0s range, which meant that the initial quake had released most of the strain that had been building-up. The largest aftershock was an M 6.2 on January 25, 2018.[12] On December 12, a 7.3 struck near the Kamchatka Peninsula with strike-slip mechanism was not part of the aftershock sequence, but was likely triggered by stress transfer from the July 17 quake.[13][5]

See also

References
  1. D. V. Chebrova, Yu. A. Kugaenkoa, A. V. Landerc, I. R. Abubakirova, A. A. Guseva, S. Ya. Drozninaa, S. V. Mityushkinaa, D. A. Ototyuka, V. M. Pavlova, and N. N. Titkova (26 April 2019). "Near Islands Aleutian Earthquake with MW = 7.8 on July 17, 2017: I. Extended Rupture along the Commander Block of the Aleutian Island Arc from Observations in Kamchatka" (PDF). Izvestiya, Physics of the Solid Earth. 55: 576–599.CS1 maint: multiple names: authors list (link)
  2. Thorne Lay, Lingling Ye, Yefei Bai, Kwok Fai Cheung, Hiroo Kanamori, Jeffrey Freymueller, Grigory M. Steblov, and Mikhail G. Kogan. "Rupture Along 400 km of the Bering Fracture Zone in the Komandorsky Islands Earthquake (MW7.8) of 17 July 2017". Geophysical Research Letters.CS1 maint: multiple names: authors list (link)
  3. "M 7.8 - Near Islands, Aleutian Islands, Alaska". US Geological Survey. Retrieved 5 Dec 2020.
  4. Donegan, Brian (17 July 2017). "Massive 7.7 Magnitude Earthquake Strikes Between Russia and Alaska". The Weather Channel. Retrieved 5 Dec 2020.
  5. E. A. Rogozhina, A. I. Lutikova, G. Yu. Dontsovab, and V. N. Zhukovets (27 August 2018). "The MW = 7.8 Earthquake of July 17, 2017 near the Commander Islands: Tectonic Position and Geodynamic Setting". Izvestiya, Physics of the Solid Earth. 55.CS1 maint: multiple names: authors list (link)
  6. Shedlock, Jerzy (17 July 2017). "No tsunami expected after large earthquake off Russia". Anchorage Daily News. Retrieved 5 Dec 2020.
  7. "Public Tsunami Message Number 2 NWS National Tsunami Warning Center Palmer AK 607 PM PDT Mon Jul 17 2017". tsunami.gov. 17 July 2017. Retrieved 5 Dec 2020.
  8. Kehoe, Kiser, H. L., E. D. (9 April 2020). "Evidence of a Supershear Transition Across a Fault Stepover". Geophysical Research Letters. 47 – via AGU.
  9. "M 6.8 - 200km NW of Attu Station, Alaska". US Geological Survey. Retrieved 5 Dec 2020.
  10. "M 6.3 - 183km ESE of Nikol'skoye, Russia". US Geological Survey. Retrieved 5 Dec 2020.
  11. "M 6.2 - 63km W of Attu Station, Alaska". US Geological Survey. Retrieved 5 Dec 2020.
  12. "M 6.2 - 48km NE of Nikol'skoye, Russia". US Geological Survey.
  13. "M 7.3 - 83km W of Nikol'skoye, Russia". US Geological Survey.
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