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Kharimkotan
Kharimkotan ((ロシア語:Харимкотан)); Japanese 春牟古丹島; Harimukotan-tō, alternatively Harumukotan-tō or 加林古丹島; Karinkotan-tō) is an uninhabited volcanic island located km from Onekotan near the northern end of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language, from “village of many Cardiocrinum”.
==Geology==
Kharimkotan is roughly oval, measuring by with an area of .〔(【引用サイトリンク】title=International Kuril Island Project（IKIP） )〕
The island consists of a dormant stratovolcano, Pik Severgin -((ロシア語: влк.Севергина ); Japanese 春牟古丹岳; ''Harikotan-dake''), which rises to above sea level. The peak is marked by two horseshoe shaped volcanic craters created by the collapse of the volcanoes upper slopes. Other evidence of the collapse can be seen on the peninsulas to the east and northwest which were formed by the debris. The volcano has erupted occasionally from the 18th century onwards, with the last recorded eruption in 1933 sending volcanic ash as far away as Paramushir. The collapse of the cone resulted in a debris-avalanche which subsequently caused a tsunami, which killed two people on Pamamushir. The path on which the debris took is visible on satellite imagery.
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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