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Cerro Solo

Solo, El

Stratovulcano · Chile-Argentina · 6205 m

Light-colored rhyodacitic pyroclastic-flow deposits blanket El Solo volcano in the Ojos del Salado area.  Snow partially mantles the summit of El Solo, a stratovolcano composed of nine eruptive centers located west of Nevados del Ojos de Salado and SE of Tres Cruces volcano.  The 6190-m-high El Solo volcano was the source of major pyroclastic-flow deposits erupted during the Holocene that thickly fill adjacent valleys.
Light-colored rhyodacitic pyroclastic-flow deposits blanket El Solo volcano in the Ojos del Salado area. Snow partially mantles the summit of El Solo, a stratovolcano composed of nine eruptive centers located west of Nevados del Ojos de Salado and SE of Tres Cruces volcano. The 6190-m-high El Solo volcano was the source of major pyroclastic-flow deposits erupted during the Holocene that thickly fill adjacent valleys. · Foto: Photo courtesy of Oscar González-Ferrán (University of Chile). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Chile-Argentina
Regione
South America Volcanic Regions / Central Andean Volcanic Arc
Altitudine
6205 m
Coordinate
-27.105, -68.713
Ultima eruzione
Sconosciuto
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Dacite
Sintesi geologica

El Solo is large stratovolcano composed of nine eruptive centers located west of Nevados del Ojos de Salado and SE of Tres Cruces volcano. The 6205-m-high volcano was the source of major rhyodacitic pyroclastic-flow deposits erupted during the Holocene that thickly fill adjacent valleys (González-Ferrán, 1995).

Sintesi da Wikipedia

Riassunto in inglese

Cerro Solo is a large stratovolcano on the border between Argentina and Chile, west of Ojos del Salado with an elevation of 6,215 metres (20,390 ft) metres. It consists of nine eruptive centers and is covered in light-colored rhyodacite pyroclastic flow deposits.

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