Gunung Kambalny
Kambalny
Stratovolkan · Russia · 2116 m

- Tipe
- Stratovolkan
- Negara
- Russia
- Wilayah
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Ketinggian
- 2116 m
- Koordinat
- 51.306, 156.875
- Letusan terakhir
- 2017
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Basalt / Picro-Basalt
Ringkasan geologi
The southernmost major stratovolcano on the Kamchatka peninsula, Kambalny has a summit crater that is breached to the SE. Five Holocene cinder cones on the W and SE flanks have produced fresh-looking lava flows. Beginning about 6,300 radiocarbon years ago, a series of major collapses of the edifice produced at least three debris-avalanche deposits. The last major eruption took place about 600 years ago, although younger tephra layers have been found, and an eruption was reported in 1767. Active fumarolic areas are found on the flanks of the volcano, which is located south of the massive Pauzhetka volcano-tectonic depression.
Ringkasan Wikipedia
Gunung Kambalny adalah sebuah gunung berapi kerucut yang terletak di bagian selatan Semenanjung Kamchatka, Rusia. Ini adalah gunung berapi aktif paling selatan di Kamchatka. Gunung ini telah meletuskan batuan mafik. Ia mempunyai kawah puncak serta lima kerucut bara di sisinya yang merupakan sumber aliran lava.
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
Garis waktu rinci
- 2017VEI 3Teramati2017-03-24 – 2017-04-23Summit crater
- 1350VEI ?Perkiraan geologi1350 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.