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Global Volcanism Program | Image GVP-07996

Volcán Telcampana, seen here from the SW, is one of a cluster of late-Pleistocene scoria cones that formed within the southern Colima graben, at the NW base of Nevado de Colima volcano. Pyroclastic surge deposits were emplaced when the cone erupted through a former lake or marsh and are exposed in roadcuts on the west side of the volcano. Photo by Jim Luhr, 1980 (Smithsonian Institution).

Volcán Telcampana, seen here from the SW, is one of a cluster of late-Pleistocene scoria cones that formed within the southern Colima graben, at the NW base of Nevado de Colima volcano. Pyroclastic surge deposits were emplaced when the cone erupted through a former lake or marsh and are exposed in roadcuts on the west side of the volcano.

Photo by Jim Luhr, 1980 (Smithsonian Institution).

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

Keywords: scoria cone


Colima