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Licancabur
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Licancabur

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Also known as Licancábur Volcano, Licancaur Volcano, Licancabur Volcano

Licancabur () is a prominent, stratovolcano on the Bolivia–Chile border in the Central Volcanic Zone of the Andes. It is capped by a summit crater which contains Licancabur Lake, a crater lake that is among the highest lakes in the world. There are no glaciers owing to the arid climate. Numerous plants and animal species live on the mountain. The volcanoes Sairecabur and Juriques are north and east of Licancabur, respectively.

Key facts

Mountain.name
Licancabur
Mountain.photo
Licancabur2.jpg
Mountain.photo_alt
A snow-capped cone rises from a desolate landscape
Mountain.elevation_m
5916
Mountain.parent_peak
Sairecabur
Mountain.isolation_parent
Sairecabur
Mountain.isolation_km
12.6
Mountain.location
Bolivia / Chile
Mountain.range
Andes
Mountain.map
Bolivia
Mountain.map_alt
Licancabur is located on the Bolivia–Chile border
Mountain.map_caption
Location of Licancabur
Mountain.type
Stratovolcano
Mountain.age
Holocene
Mountain.last_eruption
Unknown
Mountain.first_ascent
Inca, pre-Columbian
Mountain.easiest_route
Hike

via Wikipedia infobox

Wikidata facts

Elevation
5916
Image
Volcan Licancabur Bolivia.jpg
Show 2 more facts
Commons category
Licancabur
topographic prominence
1426
Sources (2)

via Wikidata · CC0

~16 min read

Article

13 sections
Contents
  • Etymology and importance
  • Geography and geomorphology
  • Geology
  • Composition
  • Climate and vegetation
  • Volcanic history
  • Archaeology and religious importance
  • Ascent
  • Notes
  • References
  • Sources
  • Bibliography
  • External links

Licancabur () is a prominent, stratovolcano on the Bolivia–Chile border in the Central Volcanic Zone of the Andes. It is capped by a summit crater which contains Licancabur Lake, a crater lake that is among the highest lakes in the world. There are no glaciers owing to the arid climate. Numerous plants and animal species live on the mountain. The volcanoes Sairecabur and Juriques are north and east of Licancabur, respectively.

Licancabur formed on top of ignimbrites produced by other volcanoes, and has been active during the Holocene. Three stages of lava flows emanated from the edifice and have a young appearance. Although no historical eruptions of the volcano are known, lava flows extending into Laguna Verde have been dated to years before present, and there may be residual heat in the mountain. The volcano has primarily erupted andesite, with small amounts of dacite and basaltic andesite.

Gallery (5)

On the map

2 mapped locations

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