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Global Volcanism Program | Image GVP-06902

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.  Photo courtesy of Oscar González-Ferrán (University of Chile).

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.

Photo courtesy of Oscar González-Ferrán (University of Chile).

Creative Commons Icon This image is made available under the Creative Commons BY-NC 4.0 license terms.


El Solo