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Tocorpuri is a volcano on the border between Chile and Bolivia. Its peak height is most recently given as and it features a wide summit crater. The volcano consists mainly of lava flows and pyroclastic deposits and is subdivided into two separate edifices. Just west of Tocorpuri, the La Torta lava dome is a high flat-topped structure. The volcanoes are formed by andesitic, dacitic and rhyolitic rocks.

Key facts

Mountain.name
Tocorpuri
Mountain.photo
Cerros de tocorpuri.jpg
Mountain.photo_caption
View from the south-west.
Mountain.other_name
Tocopuri
Mountain.elevation_m
5808
Mountain.area_km2
11
Mountain.map
Chile#Bolivia
Mountain.last_eruption
34,000 ± 7,000 years
Mountain.age
Pleistocene
Mountain.<! can't have both: volcanic_arc/belt
Central Volcanic Zone -->
Mountain.volcanic_zone
Altiplano-Puna volcanic complex

via Wikipedia infobox

Wikidata facts

Elevation
5808
Image
Tocorpuri Cerro La Torta Chile 173.jpg
Show 1 more fact
Commons category
Tocorpuri
Sources (1)

via Wikidata · CC0

~9 min read

Article

12 sections
Contents
  • Geomorphology
  • Climate and hydrology
  • Geology
  • Composition
  • Hydrothermal system
  • Geologic history
  • La Torta
  • See also
  • Notes
  • References
  • Sources
  • External links

Tocorpuri is a volcano on the border between Chile and Bolivia. Its peak height is most recently given as and it features a wide summit crater. The volcano consists mainly of lava flows and pyroclastic deposits and is subdivided into two separate edifices. Just west of Tocorpuri, the La Torta lava dome is a high flat-topped structure. The volcanoes are formed by andesitic, dacitic and rhyolitic rocks.

The Tocorpuri volcanoes developed in the late Pleistocene in three separate stages and were subject to glaciation and tectonic faulting. The most recent eruption generated the La Torta lava dome 34,000 ± 7,000 years ago; presently there is geothermal activity which may be connected to that of the neighbouring El Tatio geothermal field.

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