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

- Tipe
- Stratovolkan
- Negara
- DR Congo-Rwanda
- Wilayah
- Afrika Timur / 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
Gunung Karisimbi merupakan gunung api tidur atau tidak aktif berbentuk stratovulkan yang berada di Pegunungan Virunga, perbatasan antara negara Rwanda dengan Republik Demokratik Kongo. Di sebelah utara dari Gunung Karisimbi terdapat Gunung Mikeno, sebelah timur adalah Gunung Bisoke, serta Gunung Nyiragongo di barat. Ketinggian gunung mencapai 4.507 meter. Karisimbi merupakan gunung tertinggi di pegunungan dan gunung tertinggi kesebelas di Afrika.
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Riwayat letusan
Garis waktu rinci
- 8050 SMVEI ?Perkiraan geologiBCE 8050 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.