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Papúa Nueva Guinea · Volcán complejo

Isla Umboi

Umboi

Tipo
Volcán complejo
Altitud
1335 m
Última erupción
Desconocido
Isla Umboi
Foto: NASA Space Shuttle image STS50-99-748-47, http://eol.jsc.nasa.gov/ · Public domain · Wikimedia Commons
Tipo
Volcán complejo
País
Papúa Nueva Guinea
Región
Pacífico Suroccidental / Bismarck Volcanic Arc
Altitud
1335 m
Coordenadas
-5.592, 147.892
Última erupción
Desconocido
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Compuesto
Roca principal
Basalto / Picrobasalto
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 inglés

Umboi 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 from New Guinea's Huon Peninsula by the Vitiaz Strait. It has an elevation of 1,335 metres.

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Historial de erupciones

Glosario

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Volcanes cercanos

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.