Simbo
Stratovolcano · Solomon Islands · 335m

- Type
- Stratovolcano
- Country
- Solomon Islands
- Region
- Southwestern Pacific Volcanic Regions / Solomon Volcanic Province
- Elevation
- 335m
- Coordinates
- -8.292, 156.520
- Last eruption
- 1910
- Tectonic setting
- Subduction zone / Crustal thickness unknown
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
Simbo is a small island in the western Solomons with three truncated andesitic volcanic centers. The only Potassium-Argon date (2.3 +/- 1 million years ago from Mount Patukio) suggests a Pliocene-to-Pleistocene age for the island (Solomon Islands Geological Survey, 1982). The southern half of the island is thermally active. It contains fault-related fumarolic areas and hot springs near saltwater Lake Ove along the western coast and along the eastern coast near Mount Patukio, which has a steep-walled summit crater. Grover (1955) noted native accounts of the explosive enlargement of the Ngusunu explosion crater along the SW coast of the island one to two generations prior to 1955, probably after a visit by Guppy in 1882. Press reports mentioned an eruption in the early 1900s that forced the evacuation of villages beside Lake Ove, immediately adjacent to Ngusunu crater.
From Wikipedia
Simbo is an island in Western Province, Solomon Islands. It was known to early Europeans as Eddystone Island. The islanders have their unique language spoken nowhere else.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
- 1910 (±10 yrs)VEI ?Geological estimate1910 – OngoingNgusuna crater?
External links
⚠ For reference only. Not for emergency response.