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Copahue

File:Astronaut_Photography_of_Earth_-_Quick_View_-_Copahue_Volcano.PNG · Wikimedia Commons · See Wikimedia Commons

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Also known as Volcan Copahue

Copahue () is a stratovolcano in the Andes on the border of Bío Bío Region, Chile and Neuquén Province, Argentina. There are nine volcanic craters along a line, the easternmost of which is historically the most active, and contains a 300 m (1000 ft) wide crater lake with a pH ranging between 0.18 and 0.30. Eruptions from this crater lake have ejected pyroclastic rocks and chilled liquid sulfur fragments. Although the lake emptied during the 2000 eruption, it later returned to its previous levels. Copahue means "sulphur waters" in Mapuche.

Key facts

Mountain.name
Copahue
Mountain.photo
Astronaut Photography of Earth - Quick View - Copahue Volcano.PNG
Mountain.photo_caption
Copahue Volcano photographed from space
Mountain.elevation_m
2997
Mountain.location
Neuquén Province, Bío Bío Region,
Mountain.range
Andes
Mountain.map
Chile
Mountain.map_caption
Argentina-Chile
Mountain.map_size
200
Mountain.label_position
right
Mountain.type
Stratovolcano
Mountain.last_eruption
October 27, 2024

via Wikipedia infobox

Wikidata facts

Elevation
2997
Image
Copahue Volcano.jpg
Show 2 more facts
native label
Volcán Copahue
Commons category
Copahue Volcano
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Article

4 sections
Contents
  • See also
  • References
  • Bibliography
  • External links

Copahue () is a stratovolcano in the Andes on the border of Bío Bío Region, Chile and Neuquén Province, Argentina. There are nine volcanic craters along a line, the easternmost of which is historically the most active, and contains a 300 m (1000 ft) wide crater lake with a pH ranging between 0.18 and 0.30. Eruptions from this crater lake have ejected pyroclastic rocks and chilled liquid sulfur fragments. Although the lake emptied during the 2000 eruption, it later returned to its previous levels. Copahue means "sulphur waters" in Mapuche.

Copahue sits on a basement of sedimentary and volcanic rocks ranging in age from Eocene to Pliocene. The modern volcano sits in a volcanically active area, with a caldera from the Pliocene, measuring 20 km by 15 km, lying to the east of Copahue. The modern volcano became active roughly 1.2 million years ago (Ma). The modern caldera formed 0.6 to 0.4 Ma, and produced large pyroclastic flows, extending up to 37 km from the volcano. thumb|left|Satellite image of the December 2012 eruption The modern structure is an elongated shield volcano, with a maximum thickness of 22 km and a minimum of 8 km. It has erupted ten times since 1900, most recently in March 2016. On 27 May 2013, it was reported that a red alert had been issued and the evacuation of around 2,000 people was to begin. thumb|right|alt=The crater lake at the eastern summit of Copahue Volcano.|Copahue Crater Lake.

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On the map

3 mapped locations

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