Gunung Karisimbi
Karisimbi
Stratovolkan · DR Congo-Rwanda · 4490 m

- Tipe
- Stratovolkan
- Negara
- DR Congo-Rwanda
- Wilayah
- Eastern Africa Volcanic Regions / Albertine Rift Volcanic Province
- Ketinggian
- 4490 m
- Koordinat
- -1.506, 29.450
- Letusan terakhir
- -8050
- Kondisi tektonik
- Rift zone / Continental crust (> 25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Trachybasalt / Tephrite Basanite
Ringkasan geologi
Karisimbi is a complex basanitic-to-trachytic volcano with a symmetrical sharp-peaked summit. The 2-km-wide Branca caldera, located SE of the summit, is filled by viscous lava flows and two explosion craters. The large 1.2-km-wide Muntango pit crater is located south of the summit. A broad lava plain, formed from lava flows erupted within the caldera and along a chain of cones, extends SW. More than 100 cones erupted along a NNE-SSW zone that extends to the shores of Lake Kivu. The youngest Potassium-Argon date obtained is about 10,000 years before present (de Mulder, 1985). The youngest eruptions produced a group of dome-shaped vents east of the caldera, which fed viscous lava flows that traveled as far as 12 km E, and lava flows from the SW-flank lava vents.
Ringkasan Wikipedia
Ringkasan InggrisMount Karisimbi is a stratovolcano in the Virunga Mountains on the border between Rwanda and the Democratic Republic of Congo. At 4,507 metres (14,787 ft), Karisimbi is the highest of the eight major mountains of the mountain range, which is a part of Albertine Rift, the western branch of the East African Rift. Karisimbi is flanked by Mikeno to the north, Bisoke to the east and Nyiragongo to the west, on the other side of the Rift Valley. Karisimbi is the 11th highest mountain of Africa and ranked 61st by prominence.
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Riwayat letusan
Garis waktu rinci
- 8050 SMVEI ?Perkiraan geologiBCE 8050 – Berlangsung
Tautan eksternal
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