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Sumaco

Estratovolcán · Ecuador · 3990 m

Forested Sumaco volcano rises to 3990 m above the jungles of the western Amazon basin and is seen here in an unusually cloud-free view NE of the road from Baeza to Tena.  Sumaco is part of a north-south-trending volcanic chain far to the east of the main Andes volcanic axis and has erupted more alkaline rocks distinct from those of the main chain.  Reports of historical eruptions are somewhat ambiguous, although the volcano maintains its symmetrical shape despite heavy rainfall and intense erosion.
Forested Sumaco volcano rises to 3990 m above the jungles of the western Amazon basin and is seen here in an unusually cloud-free view NE of the road from Baeza to Tena. Sumaco is part of a north-south-trending volcanic chain far to the east of the main Andes volcanic axis and has erupted more alkaline rocks distinct from those of the main chain. Reports of historical eruptions are somewhat ambiguous, although the volcano maintains its symmetrical shape despite heavy rainfall and intense erosion. · Foto: Photo by Ursy Potter, 2005. · Wikimedia Commons
Tipo
Estratovolcán
País
Ecuador
Región
South America Volcanic Regions / Northern Andean Volcanic Arc
Altitud
3990 m
Coordenadas
-0.538, -77.626
Última erupción
1895
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Trachybasalt / Tephrite Basanite
Resumen geológico

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.

Resumen de Wikipedia

Sumaco es un estratovolcán, aislado y simétrico, que se apartó del principal eje volcánico de Ecuador. Sus rocas son muy distintos de los de la mayoría de los volcanes de los Andes debido a su falta de composición andesítica, a favor de rocas basanitas y fonolíticas. Sumaco es muy boscoso y contiene un pequeño cono en su amplio cráter de la cumbre. Una erupción histórica se produjo alrededor de 1895.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1650~1678 · 1 erupciones · VEI máx. 31876~1905 · 1 erupciones · VEI máx. 21905~1933 · 1 erupciones · VEI máx. 216501707179218481905

Línea de tiempo detallada

  1. 1933VEI 2Estimación geológica
    1933-02 – En curso
  2. 1895 (±30 años)VEI 2Observado
    1895 – En curso
  3. 1650 (±50 años)VEI 3Estimación geológica
    1650 – En curso

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.