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Volcán Lastarria

Lastarria

Estratovolcán · Chile-Argentina · 5706 m

The elongated NNW-trending edifice of 5697-m-high Lastarria volcano rises above pyroclastic-flow deposits that form an extensive apron below the northern flanks of the volcano.  Five nested craters are found along a semi-arcuate line on the summit ridge.  The youngest feature is a lava dome that overlaps the northern crater rim.  Persistent fumarolic activity occurs at the summit and NW flank, and small sulfur flows 350 m long have been produced by melting of extensive sulfur deposits in the summit region.
The elongated NNW-trending edifice of 5697-m-high Lastarria volcano rises above pyroclastic-flow deposits that form an extensive apron below the northern flanks of the volcano. Five nested craters are found along a semi-arcuate line on the summit ridge. The youngest feature is a lava dome that overlaps the northern crater rim. Persistent fumarolic activity occurs at the summit and NW flank, and small sulfur flows 350 m long have been produced by melting of extensive sulfur deposits in the summit region. · Foto: Photo by Paula Cornejo, courtesy of Oscar González-Ferrán (University of Chile). · Wikimedia Commons
Tipo
Estratovolcán
País
Chile-Argentina
Región
South America Volcanic Regions / Central Andean Volcanic Arc
Altitud
5706 m
Coordenadas
-25.168, -68.507
Última erupción
Desconocido
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The NNW-trending edifice of 5706-m-high Lastarria volcano along the Chile-Argentina border contains five nested summit craters. The youngest feature is a lava dome that overlaps the northern crater rim. The large andesitic-dacitic Negriales lava field on the western flanks was erupted from a single SW-flank vent. A large debris-avalanche deposit is found on the SE flank. Recent pyroclastic-flow deposits form an extensive apron below the northern flanks of the volcano. Although no historical eruptions have been recorded, the youthful morphology of deposits suggests activity during historical time. Persistent fumarolic activity occurs at the summit and NW flank, and sulfur flows have been produced by melting of extensive sulfur deposits in the summit region.

Resumen de Wikipedia

El Lastarria, también conocido como Azufre, es un estratovolcán enclavado en el límite entre Argentina y Chile.

Wikipedia · CC BY-SA · Leer artículo completo

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Enlaces externos

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