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Acotango is the central and highest of a group of stratovolcanoes straddling the border of Bolivia and Chile. It is high. The group is known as Kimsa Chata and consists of three mountains: Acotango, Umurata () north of it and Capurata () south of it.

Key facts

Mountain.name
Acotango
Mountain.image
Volcan Acotango and Cerro Capurata.jpg
Mountain.image_caption
The volcanoes Acotango (left) and Capurata (right)
Mountain.elevation_m
6052
Mountain.parent_peak
Guallatiri
Mountain.prominence_m
859
Mountain.listing
List of mountains in the Andes
Mountain.location
Bolivia-Chile
Mountain.range
Andes
Mountain.map
Bolivia
Mountain.map_size
250
Mountain.label_position
right
Mountain.type
Stratovolcano
Mountain.last_eruption
Pleistocene
Mountain.first_ascent
10/14/1965 (first modern ascent) - Sergio Kunstmann, Pedro Rosende and Claudio Meier (Chile)
Mountain.easiest_route
snow/ice climb

via Wikipedia infobox

Wikidata facts

Elevation
6052
Image
Acotango.jpg
Show 3 more facts
Commons category
Acotango
topographic isolation
6.19
topographic prominence
852
Sources (2)

via Wikidata · CC0

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Article

4 sections
Contents
  • First Ascent and human presence
  • See also
  • Notes
  • References

Acotango is the central and highest of a group of stratovolcanoes straddling the border of Bolivia and Chile. It is high. The group is known as Kimsa Chata and consists of three mountains: Acotango, Umurata () north of it and Capurata () south of it.

The group lies along a north–south alignment. The Acotango volcano is heavily eroded, but a lava flow on its northern flank is morphologically young, suggesting Acotango was active in the Holocene. Later research has suggested that lava flow may be of Pleistocene age. Argon-argon dating has yielded ages of 192,000±8,000 and 241,000±27,000 years on dacites from Acotango. Glacial activity has exposed parts of the inner volcano, which is hydrothermally altered. Glacial moraines lie at an altitude of but a present ice cap is only found past of altitude.

On the map

3 mapped locations

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