Harimkotan
Harimkotan is an uninhabited volcanic island located 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
Harimkotan is roughly oval, measuring by with an area of. The landscapes of the island are quite diverse. However, a significant part of the island's surface is covered with fine yellow ash, resembling desert dunes. On the northwestern cape are the ruins of an Ainu village and in the north of the island, on the shore of Severgin Bay, is the abandoned settlement of Severgino. There are a number of small freshwater lakes.Harimkotan is separated by the Sixth Kuril Strait from Onekotan, located 15 kilometers to the northeast, and by the Severgin Strait from Shiashkotan, located 29 kilometers to the south-west. There are no convenient anchorage sites.
The island consists of a dormant stratovolcano, Pik Severgin -, which rises to above sea level. The peak is marked by two horseshoe shaped volcanic craters created by the collapse of the volcano's 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.