搜尋結果
On 11 March 2011, at 14:46 JST (05:46 UTC), a Mw 9.0–9.1 undersea megathrust earthquake occurred in the Pacific Ocean, 72 km (45 mi) east of the Oshika Peninsula of the Tōhoku region. It lasted approximately six minutes and caused a tsunami. It is sometimes known in Japan as the "Great East Japan Earthquake" (東日本大震災, Higashi ...
The 2011 Tōhoku earthquake and tsunami caused a large number of displaced people. At its peak in June 2012, the number of evacuees was 346,987 [1] Some earthquake survivors died in shelters or in the process of evacuation. Many shelters struggled to feed evacuees and were not sufficiently equipped medically. [2] [3]
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Kyūshū (九州, Kyūshū, pronounced [kʲɯ ːɕɯː] , lit. 'Nine Provinces') is the third-largest island of Japan's four main islands and the most southerly of the four largest islands (i.e. excluding Okinawa). In the past, it has been known as Kyūkoku (九国, "Nine Countries"), Chinzei (鎮西, "West of the Pacified Area") and Tsukushi-no-shima (筑紫島, "Island of Tsukushi").
The Fukushima nuclear accident was a major nuclear accident at the Fukushima Daiichi nuclear power plant in Ōkuma, Fukushima, Japan which began on March 11, 2011.
Unit 731 (Japanese: 731部隊, Hepburn: Nana-san-ichi Butai), short for Manchu Detachment 731 and also known as the Kamo Detachment: 198 and the Ishii Unit, was a covert biological and chemical warfare research and development unit of the Imperial Japanese Army that engaged in lethal human experimentation and biological weapons manufacturing during the Second Sino-Japanese War (1937–1945 ...
Kumamoto (熊本市, Kumamoto-shi) is the capital city of Kumamoto Prefecture on the island of Kyushu, Japan. As of June 1, 2019, the city has an estimated population of 738,907 and a population density of 1,893 people per km 2. The total area is 390.32 km 2 . Greater Kumamoto (熊本都市圏) had a population of 1,461,000, as of the 2000 census.
v. t. e. The Richter scale [1] ( / ˈrɪktər / ), also called the Richter magnitude scale, Richter's magnitude scale, and the Gutenberg–Richter scale, [2] is a measure of the strength of earthquakes, developed by Charles Francis Richter in collaboration with Beno Gutenberg, and presented in Richter's landmark 1935 paper, where he called it ...
