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Danau Ranau

Ranau

Kaldera · Indonesia · 1854 m

Lake Ranau partially fills the 8 x 13 km Ranau caldera. A morphologically young post-caldera stratovolcano, Gunung Semuning, its summit obscured by clouds below the bottom center lake shore in this NASA Landsat image (N is to the top), was constructed within the SE side of the caldera to a height of more than 1,600 m above the caldera lake surface. The age of the most recent eruptions at Ranau are not known, but fish kills and the smell of sulfur in the late 19th and early 20th centuries may have been related to eruptions within the lake.
Lake Ranau partially fills the 8 x 13 km Ranau caldera. A morphologically young post-caldera stratovolcano, Gunung Semuning, its summit obscured by clouds below the bottom center lake shore in this NASA Landsat image (N is to the top), was constructed within the SE side of the caldera to a height of more than 1,600 m above the caldera lake surface. The age of the most recent eruptions at Ranau are not known, but fish kills and the smell of sulfur in the late 19th and early 20th centuries may have been related to eruptions within the lake. · Foto: NASA Landsat 7 image (worldwind.arc.nasa.gov) · Wikimedia Commons
Tipe
Kaldera
Negara
Indonesia
Wilayah
Sunda-Banda Volcanic Regions / 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.

Ringkasan Wikipedia

Danau Ranau adalah danau terbesar kedua di Sumatra setelah Danau Toba. Danau ini terletak di perbatasan Kabupaten Ogan Komering Ulu Selatan Provinsi Sumatera Selatan dan Kabupaten Lampung Barat Provinsi Lampung. Danau ini tercipta dari gempa besar dan letusan vulkanik dari gunung berapi yang membuat cekungan besar.

Wikipedia · CC BY-SA · Baca artikel lengkap

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1887~1889 · 1 letusan · VEI maks. ?1901~1903 · 1 letusan · VEI maks. ?18871890189518981901

Garis waktu rinci

  1. 1903VEI ?Perkiraan geologi
    1903-12-09 – 1903-12-09
  2. 1887VEI ?Perkiraan geologi
    1887-10-07 – 1888-01-20

Tautan eksternal

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