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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).

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


Puyehue-Cordón Caulle