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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.
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).
Kasatka Bay Location of Kasatka Bay in Iturup (shown in blue color). Kasatka Bay (Russian: Залив Касатка, romanized: Zaliv Kasatka), formerly known by its Japanese name Hitokappu Bay (単冠湾, Hitokappu Wan), is a natural harbor at the central part of Iturup, Kuril Islands. [1]
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.
Lake sediments overlying pumice deposits indicate that a previous caldera lake surface existed 200 m (700 ft) above sea level. The last reported explosive eruption was recorded in November 1957. This destroyed a 500 m ( 1 ⁄ 3 mi) diameter cone [ 1 ] that reportedly grew pre-eruption and had formed a peninsula extending into the lake from the ...