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Global Volcanism Program | Image GVP-07682

The eastern side of the summit of Cofre de Perote contains a steep escarpment. The volcano lies at the NNE end of a N-S-trending range that extends 50 km S to glaciated, historically active Pico de Orizaba (Citlaltépetl) in the distance. Like other N-S volcanic chains in México perpendicular to the Mexican Volcanic Belt, volcanism in the Cofre-Orizaba chain has migrated to the south. Photo by Lee Siebert, 1998 (Smithsonian Institution).

The eastern side of the summit of Cofre de Perote contains a steep escarpment. The volcano lies at the NNE end of a N-S-trending range that extends 50 km S to glaciated, historically active Pico de Orizaba (Citlaltépetl) in the distance. Like other N-S volcanic chains in México perpendicular to the Mexican Volcanic Belt, volcanism in the Cofre-Orizaba chain has migrated to the south.

Photo by Lee Siebert, 1998 (Smithsonian Institution).

Creative Commons Icon This image is made available under the Public Domain Dedication CC0 license, but proper attribution is appreciated.


Cofre de Perote