Lake Ranau
Ranau
Caldera · Indonesia · 1854m

- Type
- Caldera
- Country
- Indonesia
- Region
- Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
- Elevation
- 1854m
- Coordinates
- -4.871, 103.925
- Last eruption
- Unknown
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Caldera
- Major rock type
- Dacite
Geological summary
Ranau is an 8 x 13 km Pleistocene caldera partially filled by the crescent-shaped Lake Ranau. The caldera lies along the Great Sumatran Fault that extends the length of Sumatra. Incremental formation of the caldera culminated in the eruption of the voluminous Ranau Tuff about 0.55 million years ago. A morphologically young post-caldera stratovolcano, Gunung Semuning, was constructed within the SE side of the caldera to a height of more than 1,200 m above the lake surface. The volcano has not been mapped in sufficient detail to determine the age of its latest eruptions, although fish kills and sulfur smells in the late 19th and early 20th centuries may be related to volcanism.
From Wikipedia
This summary is short — open the full article for more detail.
Lake Ranau is a Pleistocene volcanic crater lake in Sumatra, Indonesia.
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Eruption history
Detailed timeline
- 1903VEI ?Geological estimate1903-12-09 – 1903-12-09
- 1887VEI ?Geological estimate1887-10-07 – 1888-01-20
External links
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