Isla Umboi
Umboi
Volcán complejo · Papua New Guinea · 1335 m

- Tipo
- Volcán complejo
- País
- Papua New Guinea
- Región
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- Altitud
- 1335 m
- Coordenadas
- -5.592, 147.892
- Última erupción
- Desconocido
- Contexto tectónico
- Subduction zone / Continental crust (> 25 km)
- Forma volcánica
- Composite
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
Umboi Island, 50 km in its longest dimension, is the largest of the volcanic islands off the N coast of New Guinea. Dominantly basaltic-andesitic, it is comprised of several coalescing stratovolcanoes cut by a 13 x 17 km caldera whose walls rise up to 1 km above its floor. The caldera is widely breached to the sea on the NE side and contains three youthful post-caldera cones with summit crater lakes, Talo, Soal, and Barik. Talo, displays several thermal areas and has satellitic cones on its flanks. No historical eruptions have been reported, but activity of the post-caldera cones is thought to have continued until the last few hundred years (Johnson et al., 1972).
Resumen de Wikipedia
Resumen en inglésUmboi is a volcanic island between the mainland of Papua New Guinea and the island of New Britain. It is separated from New Britain by the Dampier Strait, and Huon Peninsula and New Guinea by the Vitiaz Strait. It has an elevation of 1,335 metres.
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Historial de erupciones
Línea de tiempo detallada
No hay registros de erupciones disponibles.
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.