1995 Neftegorsk earthquake

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1995 Neftegorsk earthquake
1995 Neftegorsk earthquake is located in Far Eastern Federal District
1995 Neftegorsk earthquake
UTC time1995-05-27 13:03:53
ISC event106336
USGS-ANSSComCat
Local date27 May 1995 (1995-05-27)
Local time1:04 a.m. local time
MagnitudeMs(HRV) 7.1 [1]
Depth11.0 km (7 mi) [2]
Epicenter52°38′N 142°50′E / 52.63°N 142.83°E / 52.63; 142.83Coordinates: 52°38′N 142°50′E / 52.63°N 142.83°E / 52.63; 142.83
TypeStrike-slip[3]
Areas affectedSakhalin, Russian Far East
Total damage$64.1–300 million [3]
Max. intensityIX (Violent)[2]
Casualties1,989 dead [3]
750 injured [3]

The 1995 Neftegorsk earthquake occurred on 28 May at 1:04 local time[4] on northern Sakhalin Island in the Russian Far East.[5] It was the most destructive earthquake known within the current territory of Russia,[6] with a magnitude of Ms7.1 and maximum Mercalli intensity of IX (Violent)[7] that devastated the oil town of Neftegorsk, where 1,989 of its 3,977 citizens were killed, and another 750 injured.[8]

90% of the victims were killed by the collapse of 17 five-story residential buildings.[9] While Western media generally attributed the collapses to allegedly poor construction and shoddy materials of Soviet-era construction,[10] a geotechnical study faulted a failure to accommodate the possibility of soil liquefaction in an area that was considered "practically aseismic".[11]

The Belgian Centre for Research on the Epidemiology of Disasters' EM-DAT database places the total damage at $64.1 million, while the United States' National Geophysical Data Center assesses the damage at $300 million.[3]

This quake was not only catastrophic, it was totally unexpected: earthquakes with magnitudes greater than 6 were not known to occur in the area of northern Sakhalin Island.[12] It is also of great scientific interest (some 20 papers have been published[13]) because it occurred near a poorly known tectonic plate boundary where the Okhotsk Plate (connected with North American Plate) is crashing into the Amurian Plate (part of the Eurasian Plate),[14] and indicates that the plate boundary is associated with a north–south striking seismic belt that runs the length of Sakhalin. More precisely, this earthquake occurred on the Upper Piltoun fault (also known as the Gyrgylan'i—Ossoy fault[15]), which branches off the main that runs along the east side of the island.[16]

35 km (22 mi) of surface rupturing was observed (46 km including a branching fault), with an estimated average lateral displacement of about 4 meters, but up to 8 m (9 yd) in some places.[17] (This compares to 14 km of slip estimated to have accumulated on the Sakhalin-Hokkaido fault in the last 4 million years.[18]) The unusual strength of this quake and length of rupturing, and the low level of seismic activity beforehand, has been attributed to the accumulation of strain over a long period of time on a locked fault segment.[19]

See also[]

Notes[]

  1. ^ ISC-EB Event 106336 [IRIS] ANSS reports this as Mwb7.1.
  2. ^ a b ISC-EHB Event 106336 [IRIS].
  3. ^ a b c d e USGS (September 4, 2009), PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey
  4. ^ Klyachko 2001, p. 1.
  5. ^ ANSS: Sakhalin 1995 .
  6. ^ Arefiev et al. 2000, p. 595.
  7. ^ ISC-EHB Event 106336 [IRIS]. The ANSS: Sakhalin 1995 . reviewed value on the Mwb scale is also 7.1. Some sources have reported the magnitude as Ms 7.6.
  8. ^ Earth Chronicles (2017) attributes the fatality numbers to the Russian Ministry of Emergencies. The ISC, without citing a source, says "[a]s many as 1,989 people killed" (ISC-EHB Event 106336 [IRIS].) Other sources attribute the "more than 2000" number to Japanese language sources.
  9. ^ Klyachko 2001, p. 1. These buildings housed all but about 650 of the town's residents. Los Angeles Times 1995
  10. ^ Los Angeles Times 1995.
  11. ^ Klyachko 2001, p. 2.
  12. ^ Arefiev et al. 2000, pp. 595, 605.
  13. ^ ISC-EB Event 106336 [IRIS]
  14. ^ Arefiev et al. 2000, p. 595; Katsumata et al. 2004, pp. 117, 129.
  15. ^ Katsumata et al. 2004, p. 117
  16. ^ Arefiev et al. 2000, p. 596.
  17. ^ Arefiev et al. 2000, p. 599.
  18. ^ Arefiev et al. 2000, p. 596.
  19. ^ Arefiev et al. 2000, p. 606.

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