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The Kuril–Kamchatka Trench or Kuril Trench (Russian: Курило-Камчатский жёлоб, Kurilo-Kamchatskii Zhyolob) is an oceanic trench in the northwest Pacific Ocean. It lies off the southeast coast of Kamchatka and parallels the Kuril Island chain to meet the Japan Trench east of Hokkaido .
The Ozernaya river drains the lake. The Kurile Lake caldera is filled by the Kurile crater lake, covering a surface area of 76 square kilometres (29 sq mi) [4] to 77.1 square kilometres (29.8 sq mi). [10] A lake existed already before the Kurile Lake caldera-forming eruption. [16]
The Japan Trench is an oceanic trench part of the Pacific Ring of Fire off northeast Japan. It extends from the Kuril Islands to the northern end of the Izu Islands , and is 8,046 metres (26,398 ft) at its deepest. [ 1 ]
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 Kuril Islands or Kurile Islands [a] are a volcanic archipelago administered as part of Sakhalin Oblast in the Russian Far East. [1] The islands stretch approximately 1,300 km (810 mi) northeast from Hokkaido in Japan to Kamchatka Peninsula in Russia, separating the Sea of Okhotsk from the north Pacific Ocean .
A study by Afanas'ev et al. [8] focuses on examining the existence of the strait separating the southern and northern parts of Iturup Island in the mid-late Holocene from the perspective of coastal geomorphology. Late Pleistocene explosive volcanism is considered to have been more intense and prolonged than Early Holocene events, leading to the ...
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