Mota Lava
Motlav
성층화산 · Vanuatu · 411m

- 화산 유형
- 성층화산
- 국가
- Vanuatu
- 지역
- Southwestern Pacific Volcanic Regions / Vanuatu Volcanic Arc
- 해발
- 411m
- 좌표
- -13.670, 167.670
- 마지막 분화
- 미확인
- 판구조 환경
- Subduction zone / Intermediate crust (15-25 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
The elongated island of Motlav, also referred to as Mota Lava, is comprised of at least five Pleistocene basaltic stratovolcanoes capped by two well-preserved late-Pleistocene to Holocene pyroclastic cones, Tuntog and Vetnam. Tuntog is a largely pyroclastic composite cone at the SW end of the island with a 500-m-wide summit crater. Vetman, in the center of the island, is a pyroclastic cone truncated by a summit crater that is breached on the southern side. The 411-m high point of Motlav is a remnant of older volcanics along the central ridge of the 12-km-long, NE-SW-trending island.
Wikipedia 요약
영어 요약Mota Lava or Motalava is an island of the Banks group, in the north of Vanuatu. It forms a single coral system with the small island of Ra.
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