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Global Volcanism Program | Image GVP-10260

The Puyehue-Cordón Caulle volcanic complex forms the horizon in this view looking north across the Río Gol Gol valley from the Antillanca volcano group.  Flat-topped 2236-m-high Puyehue volcano (right) is a late-Pleistocene to Holocene basaltic-to-rhyolitic stratovolcano constructed above a 5-km-wide caldera and capped by a 2.4-km-wide summit caldera.  Historical eruptions originally attributed to Puyehue are now known to be from the Cordón Caulle rift zone, the long snow-covered ridge that extends across the photo to the left of Puyehue. Photo by Klaus Dorsch, 2001 (University of Munich).

The Puyehue-Cordón Caulle volcanic complex forms the horizon in this view looking north across the Río Gol Gol valley from the Antillanca volcano group. Flat-topped 2236-m-high Puyehue volcano (right) is a late-Pleistocene to Holocene basaltic-to-rhyolitic stratovolcano constructed above a 5-km-wide caldera and capped by a 2.4-km-wide summit caldera. Historical eruptions originally attributed to Puyehue are now known to be from the Cordón Caulle rift zone, the long snow-covered ridge that extends across the photo to the left of Puyehue.

Photo by Klaus Dorsch, 2001 (University of Munich).


Puyehue-Cordón Caulle