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・ Shōwa Genroku Rakugo Shinjū
・ Shōwa Iōjima
・ Shōwa Kenkyūkai
・ Shōwa Modan
・ Shōwa Monogatari
・ Shōwa period
・ Shōwa Restoration
・ Shōwa Station
・ Shōwa Station (Kanagawa)
・ Shōwa, Akita
・ Shōwa, Fukushima
・ Shōwa, Gunma
・ Shōwa, Saitama
・ Shōwa, Yamanashi
・ Shōwa-ku, Nagoya
Shōwa-shinzan
・ Shōwachō Station
・ Shōwachō Station (Kagawa)
・ Shōwachō Station (Osaka)
・ Shōwajima Station
・ Shōya
・ Shōyama Station
・ Shōyō-en Garden
・ Shōzaburō Watanabe
・ Shōzu District, Kagawa
・ Shōzui Station
・ Shōzō
・ Shōzō Fujii
・ Shōzō Iizuka
・ Shōzō Kitadai


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Shōwa-shinzan : ウィキペディア英語版
Shōwa-shinzan

is a volcanic lava dome in the Shikotsu-Toya National Park, Hokkaidō, Japan, next to Mount Usu. The mountain was created between 28 December 1943 and September 1945.〔神沼克伊,小山悦郎 ''日本の火山を科学する 日本列島津々浦々、あなたの身近にある108の活火山とは?'' ソフトバンククリエイティブ 2011. ISBN 978-4797361308.〕 Initially, a series of strong earthquakes shook the area, and wheat fields were rapidly uplifted. Lava broke through the surface and the current peak was created. The peak is now tall, and still actively smoking.
The name ''Shōwa-shinzan'' literally means "Showa new mountain", as it formed during the reign of Emperor Hirohito, known as the Showa period. When Shōwa-shinzan first appeared, the Japanese authorities were worried that it might be interpreted as an unlucky wartime omen, and its existence was kept secret. Much of the information about peak's formation during these years comes from local postmaster Masao Mimatsu, who kept detailed measurements of its progress.
==Volcanic Activity Timeline==
Generally, the volcanic activity of Shōwa-shinzan can be divided into three main phases as recorded by Masao Mimatsu.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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