Calabozos

Photo of this volcano
  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 35.558°S
  • 70.496°W

  • 3508 m
    11506 ft

  • 357042
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

The Global Volcanism Program has no activity reports for Calabozos.

The Global Volcanism Program has no Weekly Reports available for Calabozos.

The Global Volcanism Program has no Bulletin Reports available for Calabozos.

This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.

Eruptive History


The Global Volcanism Program is not aware of any Holocene eruptions from Calabozos. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Calabozos page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

Deformation History


There is data available for 1 deformation periods. Expand each entry for additional details.


Deformation during 2010 Feb 27 - 2010 Feb 27 [Subsidence; Observed by InSAR]

Start Date: 2010 Feb 27 Stop Date: 2010 Feb 27 Direction: Subsidence Method: InSAR
Magnitude: 14.000 cm Spatial Extent: 30.00 km Latitude: -35.000 Longitude: -71.000

Remarks: Short-lived subsidence triggered by the Mw 8.8 2010 Maule earthquake

Volcanic ground subsidence observed in interferogram stacks spanning the earthquake (with earthquake effects removed). We assume the ground displacement is of short duration compared to the interferogram time span, so we compute the stack by summing the interferograms and dividing by the number of measurements in the stack for each pixel.

From: Pritchard et al. 2013.


Reference List: Pritchard et al. 2013.

Full References:

Pritchard, M. E., J. A. Jay, F. Aron, S. T. Henderson, and L. E. Lara, 2013. Subsidence at southern Andes volcanoes induced by the 2010 Maule, Chile earthquake. Nature Geoscience, 6, p. 632-636, doi:10.1038/ngeo1855.

Emission History


There is no Emissions History data available for Calabozos.

Photo Gallery


The 26 x 14 km late-Pleistocene Calabozos caldera contains several post-caldera vents of Holocene age. The Descabezado Chico group (mid right-center) was constructed over the buried western rim of the caldera. The Cerro de Medio group (mid extreme-right) grew within the southern part of the caldera. No historical eruptions are known, but hot-spring clusters occur within the caldera.

Photo by Hugo Moreno (University of Chile).
See title for photo information.

Smithsonian Sample Collections Database


There are no samples for Calabozos in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.

Affiliated Sites