Papua New Guinea · Caldera
Lolobau Island
Lolobau
- Type
- Caldera
- Elevation
- 878m
- Last eruption
- 1912
- Type
- Caldera
- Country
- Papua New Guinea
- Region
- Southwestern Pacific / 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.
Eruption history
4 recordedGlossarySummary (VEI over time)
Click a bar to see individual eruptions · Use arrow keys to move between bars, Enter to open
Detailed timeline
- 1911VEI 4Observed1911-07-02 – 1912-07-02East flank (Sili)
- 1908VEI ?Method not stated1908-07-02 – end unknown
- 1904VEI 4Observed1904-08-09 – 1905-10-18East flank (Sili, Malo), Hulu ?
- 1100 (±30 yrs)VEI 4Geological estimate1100 – end unknownHulu
Nearby volcanoes
External links
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