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Global Volcanism Program | Image GVP-07995

Eleven scoria cones have formed in the southern Colima graben near the flanks of Colima volcano since the late Pleistocene. Cerro la Erita, a 190-m-high cone, is seen here from the NE. Cerro el Petacál (top right) is a fault block of older rocks that rises above the graben floor. Sierra Manantlán forms the 1,700-m-high western graben wall on the SW block of the rift zone. Photo by Jim Luhr, 1981 (Smithsonian Institution).

Eleven scoria cones have formed in the southern Colima graben near the flanks of Colima volcano since the late Pleistocene. Cerro la Erita, a 190-m-high cone, is seen here from the NE. Cerro el Petacál (top right) is a fault block of older rocks that rises above the graben floor. Sierra Manantlán forms the 1,700-m-high western graben wall on the SW block of the rift zone.

Photo by Jim Luhr, 1981 (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 | crater


Colima