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Kolombia · Stratovolkan

Cumbal

Tipe
Stratovolkan
Ketinggian
4764 m
Letusan terakhir
1926
Cumbal
Foto: Jorge Luis Recalde Mesías Jorgelrm · CC BY-SA 3.0 · Wikimedia Commons
Tipe
Stratovolkan
Negara
Kolombia
Wilayah
Amerika Selatan / Northern Andean Volcanic Arc
Ketinggian
4764 m
Koordinat
0.950, -77.870
Letusan terakhir
1926
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Andesit / Andesit basaltik
Ringkasan geologi

Many youthful lava flows extend from the glacier-capped Cumbal volcano, the southernmost historically active volcano of Colombia. The volcano is elongated in a NE-SW direction and is composed primarily of andesitic-dacitic lava flows. Two fumarolically active craters occupy the summit ridge: the main crater on the NE side and Mundo Nuevo crater on the SW. A young lava dome occupies the 250-m-wide summit crater, and eruptions from the upper E flank produced a 6-km-long lava field. The oldest crater lies NNE of the summit crater, suggesting SW-ward migration of activity. Explosive eruptions in 1877 and 1926 are the only known historical activity. Thermal springs are located on the SE flanks.

Ringkasan Wikipedia

Ringkasan Inggris

Cumbal is a stratovolcano of the Caribe Terrane, located at the Nudo de los Pastos in Nariño, Colombia. It is the southernmost historically active volcano of Colombia and is together with Chiles and Azufral one of the few volcanoes of the Western Ranges. The volcano is dominated by andesites.

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Riwayat letusan

2 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
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1877~1882 · 1 letusan · VEI maks. 21921~1926 · 1 letusan · VEI maks. 218771887190219111921

Garis waktu rinci

  1. 1926VEI 2Teramati
    1926-12-20 – 1926-12-21
  2. 1877VEI 2Teramati
    1877-12-16 – akhir tidak diketahui

Gunung api terdekat

Tautan eksternal

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