Due to the US Government shutdown, the Smithsonian is temporarily closed. The Global Volcanism Program website will remain available but will not be monitored or updated. Status updates will be available on the Smithsonian homepage.
Logo link to homepage

Image GVP-04853

Antuco volcano, seen here from the NW, has a complicated history beginning with construction of an andesitic stratovolcano during the Pleistocene.  Edifice failure at the beginning of the Holocene produced a large debris avalanche that traveled down the Río Laja to the west.  The collapse left a large horseshoe-shaped caldera whose NW rim forms the ridge descending to the right.  The steep-sided modern basaltic cone (upper right) has grown 1000 m since then.  Moderate explosive eruptions were recorded in the 18th and 19th centuries. Photo by Norm Banks, 1990 (U.S. Geological Survey).

Antuco volcano, seen here from the NW, has a complicated history beginning with construction of an andesitic stratovolcano during the Pleistocene. Edifice failure at the beginning of the Holocene produced a large debris avalanche that traveled down the Río Laja to the west. The collapse left a large horseshoe-shaped caldera whose NW rim forms the ridge descending to the right. The steep-sided modern basaltic cone (upper right) has grown 1000 m since then. Moderate explosive eruptions were recorded in the 18th and 19th centuries.

Photo by Norm Banks, 1990 (U.S. Geological Survey).

Creative Commons Icon This image is made available as a Public Domain Work, but proper attribution is appreciated.


Antuco