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Global Volcanism Program | Image GVP-08526

A lava flow of the Pleistocene-to-Holocene Palei-Aike volcanic field is seen here from Cerro del Diablo.  The large volcanic field straddles the Chile/Argentina border north of the Straits of Magellan.  The southernmost of the Patagonian basaltic plateau lavas, Palei-Aike contains lake-filled maars and basaltic scoria and spatter cones with associated fresh-looking lava flows.   Photo by Andres Figueroa Zurita (courtesy of Oscar González-Ferrán, University of Chile).

A lava flow of the Pleistocene-to-Holocene Palei-Aike volcanic field is seen here from Cerro del Diablo. The large volcanic field straddles the Chile/Argentina border north of the Straits of Magellan. The southernmost of the Patagonian basaltic plateau lavas, Palei-Aike contains lake-filled maars and basaltic scoria and spatter cones with associated fresh-looking lava flows.

Photo by Andres Figueroa Zurita (courtesy of Oscar González-Ferrán, University of Chile).

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Pali-Aike Volcanic Field