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The Kongō-class battlecruiser Kirishima of the Imperial Japanese Navy, and the Kongō-class guided missile destroyer Kirishima of the Japan Maritime Self-Defense Force were both named after this mountain. Shinmoedake is the most active of the Mount Kirishima volcanoes, having erupted in January 2011, March 2011, October 2017, [2] and April ...
Kirishima-Kinkowan National Park (霧島錦江湾国立公園, Kirishima-Kinkōwan Kokuritsu Kōen) is a national park in Kyūshū, Japan. It is composed of Kirishima-Kagoshima Bay, an area of Kagoshima Prefecture and Miyazaki Prefecture known for its active volcanoes, volcanic lakes, and onsen. The total area is 365.86 square kilometres (141. ...
In November, usually on the 10th, the Tenson kōrin gojinka sai (天孫降臨御神火祭) takes place there. [2] [3] It is part of the cultural area surrounding Kirishima-Jingū, a national significant cultural property, [4] [5] mainly because it was the previous site of a shrine that was destroyed by a volcanic eruption from Mount Kirishima (specifically the Takachihonomine volcano peak).
Kirishima (霧島市, Kirishima-shi) is a city located in Kagoshima Prefecture, Japan. As of 1 May 2024 [update] , the city had an estimated population of 123,640 in 63202 households, and a population density of 200 persons per km 2 .
Kirishima-Jingū (霧島神宮) is a Shinto shrine located in Kirishima, Kagoshima Prefecture, Japan. Takachiho-gawara the location of the descent from heaven is present on the shrine grounds. [1] [2] Historically, the entire of Mount Kirishima is considered part of the shrine grounds.
Karakunidake (韓国岳) or Mount Karakuni (1,700m) is a volcano in Kagoshima and Miyazaki Prefectures, Japan. It is part of Kirishima-Yaku National Park . [ 1 ] [ 3 ]
Ebino Plateau, framed by Mount Karakuni. Mount Iō (硫黄山 iōzan, lit. “Sulphur Mountain”) A field of susuki grass (Miscanthus sinensis) is located on the volcanic alluvial fan of the north-western slope of Mount Karakuni, and blooms red in autumn. The occurrence of the characteristic red hue is the result of a number of factors.
The changes in volume for the Aira and Kirishima systems suggest they had different inflation and deflation periods. Between 2009 and 2013, there was evidence of inflation in the Aira system. However, after the 2011 eruption at Kirishima, the Aira system experienced a deflation. This was Aira caldera's only deflation between 2009 and 2013. [15]