Lolobau Island
Lolobau
Caldera · Papua New Guinea · 878m
- Type
- Caldera
- Country
- Papua New Guinea
- Region
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- Elevation
- 878m
- Coordinates
- -4.916, 151.162
- Last eruption
- 1912
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Caldera
- Major rock type
- Basalt / Picro-Basalt
Geological summary
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.
From Wikipedia
Lolobau 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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Eruption history
Detailed timeline
- 1911VEI 4Observed1911 – 1912East flank (Sili)
- 1908VEI ?Geological estimate1908 – Ongoing
- 1904VEI 4Observed1904-08-09 – 1905-10-18East flank (Sili, Malo), Hulu ?
- 1100 (±30 yrs)VEI 4Geological estimate1100 – OngoingHulu
External links
⚠ For reference only. Not for emergency response.