Uratman
성층화산 · Russia · 678m
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- 화산 유형
- 성층화산
- 국가
- Russia
- 지역
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- 해발
- 678m
- 좌표
- 47.120, 152.250
- 마지막 분화
- 미확인
- 판구조 환경
- Subduction zone / Oceanic crust (< 15 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
The northernmost volcano on Simushir Island, Uratman consists of a 7.5-km-wide Pleistocene caldera with walls that rise 450 m above a 250-m-deep caldera bay. A narrow gap in the northern rim provides ocean access into Brouton Bay, which fills the NW half of the caldera. The andesitic central cone grew during the Holocene in the SE part of the caldera. Two cinder cones are located along the N flank of Uratman, and a lava dome was formed on its NW flank along Brouton Bay. No recorded eruptions are known.
Wikipedia 요약
영어 요약Uratman is a somma volcano located at the northern end of Simushir Island, Kuril Islands, Russia. It consists of a Pleistocene caldera which contains an andesite cone of Holocene age. The caldera is exposed to the ocean, forming Brouton Bay.
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