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Global Volcanism Program | Image GVP-05523

The flat-topped summit of Las Cumbres volcanic complex, a Quaternary volcano NNE of Pico de Orizaba, is seen here from the NW across the Serdán-Oriental basin. A 3.5-4.5 km wide summit caldera is partially filled by the Cerro Gordo lava dome. At least one of a group of monogenetic cones, craters, and lava domes on the flanks of the volcano is of Holocene age. Photo by Lee Siebert, 1997 (Smithsonian Institution).

The flat-topped summit of Las Cumbres volcanic complex, a Quaternary volcano NNE of Pico de Orizaba, is seen here from the NW across the Serdán-Oriental basin. A 3.5-4.5 km wide summit caldera is partially filled by the Cerro Gordo lava dome. At least one of a group of monogenetic cones, craters, and lava domes on the flanks of the volcano is of Holocene age.

Photo by Lee Siebert, 1997 (Smithsonian Institution).

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


Las Cumbres