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Kurile Lake (Russian: Кури́льское о́зеро, romanized: Kuríl'skoye Ózero) is a caldera and crater lake in Kamchatka, Russia. It is also known as Kurilskoye Lake or Kuril Lake. [3] It is part of the Eastern Volcanic Zone of Kamchatka which, together with the Sredinny Range, forms one of the volcanic belts of Kamchatka.
The Kamchatka-Kurile meadows and sparse forests ecoregion (WWF ID: PA0603) covers the coastal zones of the Kamchatka peninsula, northern section of the Kuril Islands, and the Commander Islands in the Russian Far East. The region noted for its sparse forests of Betula ermanii ("Stone birch"), and also for extensive tall-herb meadows.
The Kamchatka Peninsula [a] (Russian: полуостров Камчатка, romanized: poluostrov Kamchatka, pronounced [pəlʊˈostrəf kɐmˈt͡ɕætkə]) is a 1,250-kilometre-long (777 mi) peninsula in the Russian Far East, with an area of about 270,000 km 2 (100,000 sq mi). [3]
Tao-Rusyr Caldera (Russian: Тао-Русыр) is a stratovolcano located at the southern end of Onekotan Island, Kuril Islands, Russia.It has 7.5 km wide caldera formed during a catastrophic eruption less than 10,000 years ago (reported ages range from 5,550 to 9,400 Before Present).
The Ainu of Kunashir are South Kurils Ainu. They settled down near Kurile Lake, which was inhabited by the Kamchatka Ainu and North Kuril Ainu. In 1929, the Ainu of Kurile Lake fled to the island of Paramushir after an armed conflict with the Soviet authorities. At that time, Paramushir was under Japanese rule.
The Kamchatka–Aleutian triple junction is a triple junction of tectonic plates, of the fault–fault–trench type, where the Pacific plate, the Okhotsk plate, and the North American plate meet. [1] It is located east of the Kamchatka Mys peninsula and west of Bering Island. Meiji Seamount is located to the southeast of the junction.
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