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Irruputuncu

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Irruputuncu is a volcano in the commune of Pica, Tamarugal Province, Tarapacá Region, Chile, as well as San Pedro de Quemes Municipality, Nor Lípez Province, Potosí Department, Bolivia. The mountain's summit is high and has two summit craters—the southernmost -wide one has active fumaroles. The volcano also features lava flows, block and ash flows and several lava domes. The volcano is part of the Andean Central Volcanic Zone (CVZ).

Key facts

Mountain.name
Irruputuncu
Mountain.other_name
Iru Phutunqu, Iruputuncu, Irruputunco
Mountain.elevation_m
5163
Mountain.location
Bolivia, Potosí Department, Nor Lípez ProvinceChile, Tarapacá Region
Mountain.range
Andes, Cordillera Occidental
Mountain.map
Bolivia
Mountain.map_caption
Location in Bolivia, on the border with Chile
Mountain.label_position
right
Mountain.map_size
250
Mountain.type
Stratovolcano
Mountain.age
Pleistocene-Holocene
Mountain.last_eruption
1995

via Wikipedia infobox

Wikidata facts

Elevation
5163
Sources (2)

via Wikidata · CC0

~14 min read

Article

11 sections
Contents
  • Etymology and alternative names
  • Geography and geology
  • Regional setting
  • Local setting
  • Composition
  • Eruptive history
  • Threats and geothermal prospecting
  • Climate and vegetation
  • See also
  • References
  • External links

Irruputuncu is a volcano in the commune of Pica, Tamarugal Province, Tarapacá Region, Chile, as well as San Pedro de Quemes Municipality, Nor Lípez Province, Potosí Department, Bolivia. The mountain's summit is high and has two summit craters—the southernmost -wide one has active fumaroles. The volcano also features lava flows, block and ash flows and several lava domes. The volcano is part of the Andean Central Volcanic Zone (CVZ).

The volcano has been active during the Pleistocene and Holocene, with major eruptions occurring 258.2 ± 48.8 ka ago, between 55.9 ka and 140 ka ago and 1570 ± 900 BP (380 ± 900 AD), which were accompanied by the formation of ignimbrites. Historical volcanic activity is less clear; an eruption in 1989 is considered unconfirmed. Plumes linked to phreatomagmatic eruptive activity were observed on 26 November 1995 and 1 September 2003. Seismic activity is also observed on Irruputuncu, and ongoing fumarolic activity releasing of has left sulfur deposits in the active crater.

On the map

2 mapped locations

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