| dbo:abstract |
Many major earthquakes have occurred in the region of the Kamchatka Peninsula in far eastern Russia. Events in 1737, 1923 and 1952, were megathrust earthquakes and caused tsunamis. There are many more earthquakes and tsunamis originating from the region. (en) Полуостров Камчатка относится к сейсмически активным зонам России. Большинство камчатских землетрясений происходит на расстоянии 30—150 километров от восточного побережья полуострова, в субдукционной зоне, примыкающей к Курило-Камчатскому жёлобу. (ru) 堪察加地震是俄羅斯東部堪察加半島在1737年、1923年和1952年發生的三次大型地震，由太平洋板塊在千島海溝沉入鄂霍次克板塊引起，三次地震皆引發海嘯。 * 1737年10月16日︰震央位於座標52°30′N 159°30′E / 52.500°N 159.500°E，估計面波震級8.3Ms矩震級9.0Mw。。 * 1923年2月4日︰震央位於座標54°0′N 161°0′E / 54.000°N 161.000°E，估計矩震級8.3至8.5Mw。 * 1952年11月4日︰震央位於座標52°45′N 159°30′E / 52.750°N 159.500°E，矩震級9.0Mw。 (zh) |
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http://www.ilovekamchatka.ru/index.php%3Fshowtopic=41 https://archive.today/20130113170324/http:/beringisland.ru/quake.shtm |
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Many major earthquakes have occurred in the region of the Kamchatka Peninsula in far eastern Russia. Events in 1737, 1923 and 1952, were megathrust earthquakes and caused tsunamis. There are many more earthquakes and tsunamis originating from the region. (en) Полуостров Камчатка относится к сейсмически активным зонам России. Большинство камчатских землетрясений происходит на расстоянии 30—150 километров от восточного побережья полуострова, в субдукционной зоне, примыкающей к Курило-Камчатскому жёлобу. (ru) 堪察加地震是俄羅斯東部堪察加半島在1737年、1923年和1952年發生的三次大型地震，由太平洋板塊在千島海溝沉入鄂霍次克板塊引起，三次地震皆引發海嘯。 * 1737年10月16日︰震央位於座標52°30′N 159°30′E / 52.500°N 159.500°E，估計面波震級8.3Ms矩震級9.0Mw。。 * 1923年2月4日︰震央位於座標54°0′N 161°0′E / 54.000°N 161.000°E，估計矩震級8.3至8.5Mw。 * 1952年11月4日︰震央位於座標52°45′N 159°30′E / 52.750°N 159.500°E，矩震級9.0Mw。 (zh) |
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Kamchatka earthquakes (en) Землетрясения на Камчатке (ru) 堪察加地震 (zh) |
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