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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).


Cofre de Perote