Logo link to homepage

Global Volcanism Program | Image GVP-12080

Conical Volcán Chiliques (left) and Volcan Miscanti (right) rise to the NE above Laguna Miscanti.  The 5778-m-high summit of Chiliques contains a 500-m-wide crater, and some youthful lava flows may be of Holocene age. This volcano had previously been considered to be dormant; however, in 2002 a NASA nighttime thermal infrared ASTER satellite image showed low-level hot spots in the summit crater and upper flanks.  Miscanti volcano is of probable late-Pleistocene age.  Photo by Jos Offermans, 2008.

Conical Volcán Chiliques (left) and Volcan Miscanti (right) rise to the NE above Laguna Miscanti. The 5778-m-high summit of Chiliques contains a 500-m-wide crater, and some youthful lava flows may be of Holocene age. This volcano had previously been considered to be dormant; however, in 2002 a NASA nighttime thermal infrared ASTER satellite image showed low-level hot spots in the summit crater and upper flanks. Miscanti volcano is of probable late-Pleistocene age.

Photo by Jos Offermans, 2008.


Chiliques

Miscanti