Lolobau Island
Lolobau
Caldera · Papua New Guinea · 878 m
- Tipo
- Caldera
- País
- Papua New Guinea
- Región
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- Altitud
- 878 m
- Coordenadas
- -4.916, 151.162
- Última erupción
- 1912
- Contexto tectónico
- Subduction zone / Continental crust (> 25 km)
- Forma volcánica
- Caldera
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
Lolobau volcano has grown over the W rim of a 6-km-wide caldera which formed about 12,000 years ago. The 8 x 13 km island is located just off the coast of eastern New Britain. A small lake occupies the SW part of the caldera. A small lava dome (Hulu) caps Mount Lolobau, which has a 0.8 x 1.1 km summit crater breached to the NE. Flank cones are found along the coast of the largely submerged volcano. Several vents within the caldera, on the E flank of the main edifice, have been active during historical time. The latest eruptions took place during the early 20th century.
Resumen de Wikipedia
Resumen en inglésLolobau Island is an island in the Bismarck Sea, within the West New Britain Province of the Islands Region, in northern Papua New Guinea.
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Historial de erupciones
Línea de tiempo detallada
- 1911VEI 4Observado1911 – 1912East flank (Sili)
- 1908VEI ?Estimación geológica1908 – En curso
- 1904VEI 4Observado1904-08-09 – 1905-10-18East flank (Sili, Malo), Hulu ?
- 1100 (±30 años)VEI 4Estimación geológica1100 – En cursoHulu
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.