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Global Volcanism Program | Image GVP-08423

The eroded Plio-Pleistocene Ixhuatán volcano rises to the NE above the Pacific coastal plain of Guatemala.  Ixhuatán has produced dominantly andesitic lava flows and volcaniclastic deposits.  NE-SW-trending faults cut the volcanic complex.  Pleistocene andesitic ignimbrite deposits from the neighboring Tecuamburro volcanic complex bank up onto the western flanks of Ixhuatán. Photo by Lee Siebert, 1988 (Smithsonian Institution).

The eroded Plio-Pleistocene Ixhuatán volcano rises to the NE above the Pacific coastal plain of Guatemala. Ixhuatán has produced dominantly andesitic lava flows and volcaniclastic deposits. NE-SW-trending faults cut the volcanic complex. Pleistocene andesitic ignimbrite deposits from the neighboring Tecuamburro volcanic complex bank up onto the western flanks of Ixhuatán.

Photo by Lee Siebert, 1988 (Smithsonian Institution).

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


Ixhuatán