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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 44.3°S
  • 72.53°W

  • 524 m
    1719 ft

  • 358053
  • Latitude
  • Longitude

  • Summit

  • Volcano

There are no activity reports for Puyuhuapi.

 Available Weekly Reports

There are no Weekly Reports available for Puyuhuapi.

There are no Holocene eruptions known for Puyuhuapi. 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.

Fuenzalida R, Etchart H, 1976. Evidencias de migracion volcanica reciente desde la linea de volcanes de la Patagonia Chilena. In: Gonzalez-Ferran O (ed) {Proc Symp Andean & Antarctic Volcanology Problems (Santiago, Chile, Sept 1974)}, Rome: IAVCEI, p 392-397.

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

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

A chain of dominantly basaltic cinder cones erupted along two NE-SW-trending fissures at the head of Puyuhuapi fjord comprise the Volcanes de Puyuhuapi. The larger group of four cones lies on the western side of Puyuhuapi fjord and fed lava flows that traveled SE to the sea. The second lineament formed a chain of four smaller cones between the head of the fjord and Lake Risopatrón to the north. The two fractures are related to the regional Liquiñe-Ofqui fault zone. The Puyuhuapi cinder cones are extremely well preserved, suggesting a very young age.