Danau Ranau
Ranau
Kaldera · Indonesia · 1854 m

- Tipe
- Kaldera
- Negara
- Indonesia
- Wilayah
- Sunda & Banda / Sunda Volcanic Arc
- Ketinggian
- 1854 m
- Koordinat
- -4.871, 103.925
- Letusan terakhir
- Tidak diketahui
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Caldera
- Batuan utama
- Dacite
Ringkasan geologi
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.
Riwayat letusan
Garis waktu rinci
- 1903VEI ?Perkiraan geologi1903-12-09 – 1903-12-09
- 1887VEI ?Perkiraan geologi1887-10-07 – 1888-01-20
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.