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Image GVP-07212

The broad massif of Cerro Cacahuatique lies in the interior valley of El Salvador about 30 km NNE of San Miguel volcano.  The massive 1500-m-high Pleistocene stratovolcano (also spelled Cerro Cacaguatique) rises 1000 m above its base and is deeply dissected, although it still retains its subdued conical form.  A large erosional caldera, formed through a breach on the SE side, truncates the summit.   Photo by Carlos Pullinger, 1999 (Servicio Nacional de Estudios Territoriales, El Salvador).

The broad massif of Cerro Cacahuatique lies in the interior valley of El Salvador about 30 km NNE of San Miguel volcano. The massive 1500-m-high Pleistocene stratovolcano (also spelled Cerro Cacaguatique) rises 1000 m above its base and is deeply dissected, although it still retains its subdued conical form. A large erosional caldera, formed through a breach on the SE side, truncates the summit.

Photo by Carlos Pullinger, 1999 (Servicio Nacional de Estudios Territoriales, El Salvador).

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Cerro Cacahuatique