파푸아뉴기니 · 다봉화산
Takuan Group
- 화산 유형
- 다봉화산
- 해발
- 2210m
- 마지막 분화
- 미확인

- 화산 유형
- 다봉화산
- 국가
- 파푸아뉴기니
- 지역
- 남서태평양 / Bougainville Volcanic Arc
- 해발
- 2210m
- 좌표
- -6.442, 155.608
- 마지막 분화
- 미확인
- 판구조 환경
- 섭입대 / 지각 두께 미상
- 화산 지형
- 복성화산체
- 주요 암석
- 안산암 / 현무암질 안산암
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.
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