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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 23.58°S
  • 67.7°W

  • 5778 m
    18952 ft

  • 355098
  • Latitude
  • Longitude

  • Summit

  • Volcano

There are no activity reports for Chiliques.

 Available Weekly Reports

There are no Weekly Reports available for Chiliques.

There are no Holocene eruptions known for Chiliques. If this volcano has had large eruptions prior to 10,000 years ago, information might be found in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

de Silva S L, 2007. . (pers. comm.).

de Silva S L, Francis P W, 1991. Volcanoes of the Central Andes. Berlin: Springer-Verlag, 216 p.

Gonzalez-Ferran O, 1995. Volcanes de Chile. Santiago: Instituto Geografico Militar, 635 p.

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Moreno H, 1985. . (pers. comm.).

Volcán Chiliques is a structurally simple stratovolcano located immediately south of Laguna Lejía. The 5778-m-high summit contains a 500-m-wide crater. Several youthful lava flows, some of which are considered to be of possible Holocene age (de Silva, 2007 pers. comm.), descend its flanks. The largest of these extends 5 km to the NW. Older lava flows reach up to 10 km from the summit on the north flank. This volcano had previously been considered to be dormant; however, in 2002 a NASA nighttime thermal infrared satellite image from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) showed low-level hot spots in the summit crater and upper flanks.