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意味・対訳 安政の大地震(あんせいのおおじしん/だいじしん)は、江戸時代後期の安政年間(1850年代)に、日本各地で連発した大地震である。
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Namazue: Pictures that appeared after the Ansei Great Earthquakes.発音を聞く 例文帳に追加
鯰絵安政の大地震後に登場した絵。 - Wikipedia日英京都関連文書対訳コーパス
He lost his wife and children in the Ansei Great Earthquakes in 1855, but he made nishikie (colored woodblock prints) of disastrous scenes of Yoshiwara and he became famous.発音を聞く 例文帳に追加
1855年(安政2年)、安政の大地震で妻子を失うが、この時の吉原の惨状を錦絵に描き名を挙げる。 - Wikipedia日英京都関連文書対訳コーパス
However, when Toko was killed by the Ansei Great Earthquakes in 1855, the dispute, without a mediator, quickly became mired in a mess.発音を聞く 例文帳に追加
しかし、1855年に発生した安政の大地震にて東湖が圧死すると調停役を失った抗争は一気に泥沼化。 - Wikipedia日英京都関連文書対訳コーパス
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ウィキペディア英語版での「Ansei Great Earthquakes」の意味 |
Ansei Great Earthquakes
出典:『Wikipedia』 (2011/01/30 00:14 UTC 版)
The Ansei Great Earthquakes (安政の大地震, Ansei no Dai Jishin) were a series of three major earthquakes that struck Japan during the Ansei era (1854–1860).
- The Ansei-Tōkai Quake (安政東海地震, Ansei Tōkai Jishin) was an 8.4 magnitude earthquake which struck on December 23, 1854. The epicenter ranged from Suruga Bay to the deep ocean, and struck primarily in the Tōkai region, but destroyed houses as far away as in Edo. The accompanying tsunami caused damage along the entire coast from the Bōsō Peninsula in modern-day Chiba prefecture to Tosa province (modern-day Kōchi prefecture)
- The Ansei-Nankai Quake (安政南海地震, Ansei Nankai Jishin) was an 8.4 magnitude earthquake which struck on December 24, 1854. Over 10,000 people from the Tōkai region down to Kyushu were killed.
- The Ansei Edo Quake (安政江戸地震, Ansei Edo Jishin) was a 6.9 magnitude earthquake which struck Edo (modern-day Tokyo) on November 11, 1855. One hundred and twenty earthquakes and tremors in total were felt in Edo in 1854-55. The great earthquake struck after 10 o'clock in the evening; roughly 30 aftershocks continued until dawn. The epicenter was near the mouth of the Arakawa River. Records from the time indicate 6,641 deaths inside the city, and 2,759 injuries; much of the city was destroyed by fire, leading many people to stay in rural inns. Aftershocks continued for twenty days. This quake was a particularly destructive deep thrust quake caused by a giant slab of rock stuck between the Philippine Sea Plate and the Pacific Plate.
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Text is available under Creative Commons Attribution-ShareAlike (CC-BY-SA) and/or GNU Free Documentation License (GFDL). Weblio英和・和英辞典に掲載されている「Wikipedia英語版」の記事は、WikipediaのAnsei Great Earthquakes (改訂履歴)の記事を複製、再配布したものにあたり、Creative Commons Attribution-ShareAlike (CC-BY-SA)もしくはGNU Free Documentation Licenseというライセンスの下で提供されています。 |
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