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Global Volcanism Program | Image GVP-06888

Volcán Chiliques, the conical peak at the left, is a structurally simple stratovolcano located immediately south of Laguna Lejía.  A 500-m-wide snow-capped crater truncates the summit and contains a small lake.  The volcano was constructed over a base of dacitic lava domes and andesitic lava flows.  Youthful lava flows radially descended from the summit as far as 5 km to the NW.  The volcanic complex at the right is the Pleistocene Volcán Lejía, which was constructed within a 3.5-km-wide caldera. Photo by Instituto Geográfico Militar, courtesy of Oscar González-Ferrán (University of Chile).

Volcán Chiliques, the conical peak at the left, is a structurally simple stratovolcano located immediately south of Laguna Lejía. A 500-m-wide snow-capped crater truncates the summit and contains a small lake. The volcano was constructed over a base of dacitic lava domes and andesitic lava flows. Youthful lava flows radially descended from the summit as far as 5 km to the NW. The volcanic complex at the right is the Pleistocene Volcán Lejía, which was constructed within a 3.5-km-wide caldera.

Photo by Instituto Geográfico Militar, courtesy of Oscar González-Ferrán (University of Chile).

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Chiliques

Lejía