1841 Kamchatka earthquake

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1841 Kamchatka earthquake
1841 Kamchatka earthquake is located in Kamchatka Krai
1841 Kamchatka earthquake
Epicenter marked as a bullseye.
UTC time21:30
Local dateMay 17, 1841 (1841-05-17)
Local time08:00
Magnitude9.0+ Mw
9.0+ Mt 
8.4 Mfa
Epicenter52°30′N 159°30′E / 52.5°N 159.5°E / 52.5; 159.5Coordinates: 52°30′N 159°30′E / 52.5°N 159.5°E / 52.5; 159.5
TypeMegathrust
Areas affectedKamchatka
Max. intensityMSK-64 IX (Destructive)
Tsunami15 meters
AftershocksUntil March 1842
CasualtiesUnknown

The 1841 Kamchatka earthquake occurred in the Pacific Ocean on May 17 at 08:00 local time. The earthquake had an epicenter off the Russian Far East's Kamchatka Peninsula. With an estimated moment magnitude of 9.0 or higher, it is one of the largest to strike the region. A large tsunami accompanied the quake, with up to 15 meters in run-up along the coast.

Tectonic setting[]

The earthquake occurred off the Kamchatka Peninsula's east coast, which runs parallel to the Kuril-Kamchatka Trench, the area where the Pacific and Okhotsk Sea plates converge. Being older and therefore denser, the Pacific subducts beneath the Kamchatka Peninsula, which sits on the Okhotsk Sea Plate. These two plates meet along a convergent boundary, marked by the trench. The subduction zone is seismogenic and produces Kamchatka earthquakes, which occasionally generate tsunamis; some of these megathrust earthquakes are very strong (such as the 1952 magnitude 9.0 earthquake, the 5th largest ever recorded).[1] Possibly the largest to have hit the peninsula was the 1737 magnitude 9.3 earthquake which generated a large tsunami as well.[2]

Earthquake[]

The earthquake was associated with thrust faulting on the subduction zone near the east coast of the Kamchatka Peninsula. According to the National Centers for Environmental Information, the earthquake's magnitude at Mfa  8.4 using the felt area to determine its size. A 2004 earthquake catalog placed both the tsunami magnitude (Mt ) and moment magnitude (Mw ) at 9.0, based on evaluating the available tsunami data.[3][4] No information exists on the source area of the event due to the lack of tsunami records and observation.[5] The 1841 event is thought to be one of a number of large M 8.5+ earthquakes "missing" in the seismological record due to having their magnitudes underestimated. According to Dr. Susan Hough of the U.S. Geological Survey, the earthquake magnitude was underestimated due to the assumption that it did not generate a large-enough tsunami. Earthquakes measuring 8.5 or greater are generally assumed to cause large tsunamis. At the American Geophysical Union fall meeting in 2013, she believes the magnitude could be up to 9.2.[6]

Tsunami[]

The event caused a large tsunami with a maximum run-up height of 15 meters at the eastern coast.[7] The tsunami washed away yurts belonging to the native population.[8] At Hilo, Hawaii, the tsunami was measured at 4.6 meters. It is Hawaii's first historically recorded tsunami sourced from the Kamchatka Peninsula.[9]

Damage[]

The earthquake struck the coast and was felt with a maximum intensity of VIII–IX at Petropavlovsk-Kamchatskiy.[3] Up to 15 minutes of violent shaking was felt in the city. At least 50 stove chimneys on homes and government offices collapsed. Some homes suffered severe damage.[10] Cliffs at the coast collapsed. Cathedral bells reportedly rang during the quake.[8]

See also[]

References[]

  1. ^ "20 Largest Earthquakes in the World". www.usgs.gov. Retrieved 2021-06-20.
  2. ^ Chubarov L.B.; V. K. Gusiakov. "Tsunamis and earthquake mechanism in the island arc region". Science of Tsunami Hazards. 3 (1): 3–21.
  3. ^ a b Alexander A Gusev; L.S. Shumilina (2004). "Recurrence of Kamchatka strong earthquakes on a scale of moment magnitudes" (PDF). Izvestiya Physics of the Solid Earth. 40 (3): 206–215.
  4. ^ Breanyn T. MacInnes; Robert Weiss; Joanne Bourgeois; Tatiana K. Pinegina (2010). "Slip Distribution of the 1952 Kamchatka Great Earthquake Based on Near-Field Tsunami Deposits and Historical Records" (PDF). Bulletin of the Seismological Society of America. 100 (4): 1695–1709. doi:10.1785/0120090376.
  5. ^ Thorne Lay; Hiroo Kanamori; Larry Ruff (1982). "The Asperity Model and the Nature of Large Subduction Zone Earthquakes" (PDF). Earthquake Prediction Research. 1 (1): 3–71. ISSN 0286-0619.
  6. ^ Rebecca Morelle (12 December 2013). "Enormous earthquakes 'are missing' from records". BBC News. Retrieved 23 October 2021.
  7. ^ Joanne Bourgeois; Tatiana K. Pinegina (2017). "The 1997 Kronotsky earthquake and tsunami and their predecessors, Kamchatka, Russia" (PDF). Natural Hazards and Earth System Sciences. 18: 335–350. doi:10.5194/nhess-18-335-2018.
  8. ^ a b "ЗЕМЛЕТРЯСЕНИЕ 17 МАЯ 1841 г." [EARTHQUAKE MAY 17, 1841]. wdcb.ru (in Russian). World Data Center for Solid Earth Physics. Retrieved 23 October 2021.
  9. ^ "Tsunami Event Information". ngdc.noaa.gov. NOAA National Centers for Environmental Information. Retrieved 23 October 2021.
  10. ^ "Significant Earthquake Information". ngdc.noaa.gov. NOAA National Centers for Environmental Information. Retrieved 23 October 2021.
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