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Ekuador · Stratovolkan

Sumaco

Tipe
Stratovolkan
Ketinggian
3990 m
Letusan terakhir
1895
Sumaco
Foto: Sylvain2803 · CC BY-SA 3.0 · Wikimedia Commons
Tipe
Stratovolkan
Negara
Ekuador
Wilayah
Amerika Selatan / Northern Andean Volcanic Arc
Ketinggian
3990 m
Koordinat
-0.538, -77.626
Letusan terakhir
1895
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Trakibasal / Tefrit basanit
Ringkasan geologi

The forested Sumaco stratovolcano rises above the jungles of the western Amazon basin, east of Antisana volcano, and occupies an isolated position far to the east of the main Andes volcanic axis. Constructed over Cretaceous sedimentary rocks, it forms a relatively symmetrical cone in an area of heavy rainfall and erosion. Sumaco has produced alkaline tephritic, basanitic, and phonolitic rocks distinct from those of the main Andean chain. The volcano has a broad summit crater, 300 x 400 m wide, containing a central cone. Reports of historical eruptions are somewhat ambiguous; an eruption is inferred in the 18th or early-19th century on the basis of changes in crater morphology.

Ringkasan Wikipedia

Ringkasan Inggris

Sumaco is a symmetrical, isolated stratovolcano, that is set off from the main Ecuador volcanic axis. Its rocks are very distinct from those from most Andean volcanoes because of its lack of andesitic composition, in favour of basanite and phonolitic rock. Sumaco is heavily forested and contains a small cone in its broad summit crater. An historical eruption occurred around 1895.

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Riwayat letusan

3 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu · Gunakan tombol panah untuk berpindah batang, Enter untuk membuka
1650~1678 · 1 letusan · VEI maks. 31876~1905 · 1 letusan · VEI maks. 21905~1933 · 1 letusan · VEI maks. 216501707179218481905

Garis waktu rinci

  1. 1933VEI 2Metode tidak dinyatakan
    1933-02-16 – akhir tidak diketahui
  2. 1895 (±30 tahun)VEI 2Teramati
    1895-07-02 – akhir tidak diketahui
  3. 1650 (±50 tahun)VEI 3Metode tidak dinyatakan
    1650 – akhir tidak diketahui

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