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Cuernos del Diablo
"Cuernos del Diablo is a 1862-m-high partially glacially eroded basaltic stratovolcano. Numerous satellitic pyroclastic cones and associated basaltic lava flows were formed during the Holocene, principally on the SW flank and from the summit to the NW base of the volcano. Although no historical eruptions are known from Cuernos del Diablo, some of these cones may have formed during historical time (González-Ferrán, 1995). Fumaroles were observed on a flank cone in 1931."  -Smithsonian Volcano Archive
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