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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Chirinkotan ： ウィキペディア英語版 Chirinkotan Chirinkotan ((ロシア語:Чиринкотан); Japanese 知林古丹島; Chirinkotan-tō) is an uninhabited volcanic island located in the centre of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language for "mudslide". It is located 30 kilometers west of Ekarma, its nearest neighbor. ==Geology== Chirinkotan is at the far end of a volcanic chain extending nearly 50 km west of the central part of the main Kuril Islands arc. The island is the top of a partially submerged stratovolcano rising approximately 3000 meters from the floor of the Sea of Okhotsk, and is roughly circular with an area of 6 km² 〔(【引用サイトリンク】title=International Kuril Island Project（IKIP） )〕 The island’s highest point (“Masaochi” in Ainu) is 742 meters high, is still active volcano with major eruptions recorded in 1760, 1884, 1900, 1979, 1986, 2004, and 2013. Reports of a 1955 eruption are unconfirmed. The caldera is approximately one kilometer wide, with a depth of 300 to 400 meters, and is breached on its south-east side. The shores of the island are steep cliffs, making landing by small boat impossible. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Chirinkotan」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.