Lolobau Island
Lolobau
Caldera · Papua New Guinea · 878 m
- Tipo
- Caldera
- Paese
- Papua New Guinea
- Regione
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- Altitudine
- 878 m
- Coordinate
- -4.916, 151.162
- Ultima eruzione
- 1912
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Caldera
- Roccia principale
- Basalt / Picro-Basalt
Sintesi geologica
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.
Sintesi da Wikipedia
Riassunto in ingleseLolobau 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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Storia delle eruzioni
Cronologia dettagliata
- 1911VEI 4Osservata1911 – 1912East flank (Sili)
- 1908VEI ?Stima geologica1908 – In corso
- 1904VEI 4Osservata1904-08-09 – 1905-10-18East flank (Sili, Malo), Hulu ?
- 1100 (±30 anni)VEI 4Stima geologica1100 – In corsoHulu
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.