Takuan Group
집합화산 · Papua New Guinea · 2210m

- 화산 유형
- 집합화산
- 국가
- Papua New Guinea
- 지역
- Southwestern Pacific Volcanic Regions / Bougainville Volcanic Arc
- 해발
- 2210m
- 좌표
- -6.442, 155.608
- 마지막 분화
- 미확인
- 판구조 환경
- Subduction zone / Crustal thickness unknown
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
The Takuan volcano group in southern Bougainville Island consists of three closely spaced, NW-SE-trending andesitic-dacitic stratovolcanoes. Two of these are relatively uneroded and have probably been active during the Holocene, and a third, extensively eroded volcano is probably Pleistocene in age (Blake and Meizitis, 1967). Along with Loloru volcano, the Takuan volcanoes are post-caldera cones constructed along the rim of the Pleistocene Laluai caldera. The 2210-m NW-most volcano, Mount Takuan, is the highest of the group and is a lava cone that has fed viscous lavas flows to the south, similar to those at Bagana volcano. The central volcano contains a large lava dome in its breached summit crater; this dome may represent the most recent activity of the Takuan volcano group. Older, but still well-preserved lava flows are found on the flanks of this volcano.
Wikipedia 요약
영어 요약Takuan Group is a volcanic group located in the southern part of Bougainville Island, Papua New Guinea. It consists of three closely spaced stratovolcanoes and lava cones, Mount Takuan being the highest of them.
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