Английская Википедия:1922 Vallenar earthquake

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The 1922 Vallenar earthquake occurred with a moment magnitude of 8.5–8.6 and a tsunami magnitude of 8.7 in the Atacama Region of Chile, near the border with Argentina on 11 November at 04:32 UTC.[1][2][3][4] It triggered a destructive tsunami that caused significant damage to the coast of Chile and was observed as far away as Australia.

Tectonic setting

The earthquake took place along the boundary between the Nazca and South American tectonic plates, at a location where they converge at a rate of seventy millimeters a year.

Chile has been at a convergent plate boundary that generates megathrust earthquakes since the Paleozoic (500 million years ago). In historical times the Chilean coast has suffered many megathrust earthquakes along this plate boundary, including the strongest earthquake ever measured. Most recently, the boundary ruptured in 2010 in central Chile.[5]

Damage and deaths

The earthquake caused extensive damage in a zone extending approximately from Copiapó to Coquimbo. Newspapers estimated more than 1,000 dead as a result of the quake, at least 500 of them in Vallenar.[6] The tsunami killed several hundred people in coastal cities, especially in Coquimbo.[1]

Total damage was estimated to be in the range of $5–25 million U.S. (1922 dollars).[1][7]

Characteristics

Earthquake

Файл:Casas colapsadas por terremoto de Vallenar de 1922.jpg
Damage in the Atacama Region

The earthquake was preceded by strong foreshocks on 3 and 7 November. The main shock lasted between thirty seconds and eight minutes according to various reports.[8] A maximum Mercalli-Sieberg intensity was XI assigned in Vallenar and the surrounding region was assigned X. Shaking intensity decreased further west towards the coast, ranging from VII to IX. The location closest to the tsunami source, Caldera, was assigned VII. This suggest an inland earthquake source.[9]

The length of the plate boundary that ruptured during the earthquake is estimated to be 390 km (242 mi).[10]

Tsunami

The epicenter of the earthquake was well inland and the tsunami may have been caused by a submarine slide triggered by the shaking.[11]

At Caldera the tsunami began about 15 minutes after the earthquake, with a maximum run-up height of 7 m (23 ft). At Chañaral the tsunami had three surges, the first about an hour after the earthquake, the maximum run-up height was 9 m (30 ft). Three surges were also seen at Coquimbo, the last being the most destructive with a maximum run-up of 7 m (23 ft).[10]

The tsunami was also observed in Callao, Peru (2.4 m, 7.9 ft), California (0.2 m, 8 in 13.0 hours delay), Hawaii (2.1 m, 6.9 ft 14.5 hours), Samoa (0.9 m, 3 ft 14.1 hours), Japan (0.3 m, 1 ft), Taiwan (0.03 m, 1 in), New Zealand (0.1 m, 3.9 in), Australia (0.2 m, 7.9 in)[12] and the Philippines (0.1 m, 3.9 in).[8]

See also

References

Шаблон:Reflist

External links

Шаблон:Earthquakes in Chile

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  1. ↑ 1,0 1,1 1,2 USGS, Historic Earthquakes.Chile-Argentina Border. 1922 November 11 04:32 UTC. Magnitude 8.5
  2. ↑ Seismological Notes, Bulletin of the Seismological Society of America. "Seismological Notes" is a list of recent important earthquakes with short summaries included in each issue of the BSSA.
  3. ↑ Шаблон:Cite journal
  4. ↑ Шаблон:Cite journal
  5. ↑ Шаблон:Cite web
  6. ↑ "Thousands Die in Earthquake." Tulsa (OK) World, 13 November 1922, p. 1.
  7. ↑ Dunbar, Paula K., Lockridge, Patricia A., and Whiteside, Lowell S., 1992, Catalog of significant earthquakes 2150 B.C. – 1991 A.D.: U. S. Dept. of Commerce, National Oceanic and Atmospheric Administration.
  8. ↑ 8,0 8,1 Шаблон:Cite web
  9. ↑ Шаблон:Cite journal
  10. ↑ 10,0 10,1 Шаблон:Cite web
  11. ↑ Шаблон:Cite journal
  12. ↑ Шаблон:Cite web
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