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Satellite image showing the plume from Puyehue yesterday (thanks to Sergio Abarca Delgad ‏@sergio_raptor / Twitter)
Friday, Jan 17, 2014
A small emission of gas and some ash was reported by Buenos Aires VAAC. In fact, a diluted plume of gas, steam, and possibly some volcanic ash is visible on satellite images from yesterday and this morning. ... [mehr]
MODIS / Terra satellite image 14 Dec showing a plume drifting N from Puyehue
Sunday, Dec 15, 2013
A significant ash(?) plume was spotted on Terra's satellite images yesterday afternoon. Since there are no other reports suggesting that a (larger in this case) eruption has occurred (e.g. heat signals, eyewitness reports, webcam), it seems likely that the plume was from wind-mobilized ash from the 2011-12 eruption. ... [mehr]

Puyehue-Cordón Caulle Vulkan

Schichtvulkan 2236 m / 7,336 ft
Argentinien/Chile (Zentrum), South America, -40.59°S / -72.12°W
Aktueller Status: normal / ruhend (1 von 5)
Puyehue-Cordón Caulle Webcams / aktuelle Daten | Berichte
Puyehue-Cordón Caulle Vulkan-B cher
Last update: 19 Aug 2018
Typische Aktivität: explosive
Ausbrüche des Puyehue-Cordón Caulle: 1960, 1934, 1929, 1921-22, 1905(?), 1893(?) Puyehue-Cordón Caulle with the steam and ash plume from the rift zone eruption seen from space on 26 January 2012 (NASA Earth Observatory)No recent earthquakes
UhrzeitMag. / TiefeDistanceOrt
Puyehue-Cordón Caulle volcano in Central Chile is a complex of 2 volcanoes: Puyehue volcano and the fissure system of Cordón Caulle. Puyehue volcano has a 2.4 km wide summit caldera, but historical eruptions occurred at the Cordón Caulle rift zone.
The Cordón Caulle geothermal area occupies a 6 x 13 km wide depression and is the largest active geothermal area in the southern Andes.
Neighboring Calbuco and Puyehue volcanoes lie on the same traverse fault and is has been noted that they tend at the same time or within only few years distance.


The Puyehue-Cordón Caulle volcanic complex (PCCVC) is a large NW-SE-trending late-Pleistocene to Holocene basaltic-to-rhyolitic transverse volcanic chain SE of Lago Ranco.
The 1799-m-high Pleistocene Cordillera Nevada caldera lies at the NW end, separated from Puyehue stratovolcano at the SE end by the Cordón Caulle fissure complex. The Pleistocene Mencheca volcano with Holocene flank cones lies NE of Puyehue.
The basaltic-to-rhyolitic Puyehue volcano is the most geochemically diverse of the PCCVC. The flat-topped, 2236-m-high Puyehue volcano was constructed above a 5-km-wide caldera and is capped by a 2.4-km-wide summit caldera of Holocene age.
Lava flows and domes of mostly rhyolitic composition are found on the eastern flank of Puyehue. Historical eruptions originally attributed to Puyehue, including major eruptions in 1921-22 and 1960, are now known to be from the Cordón Caulle rift zone.
Source: USGS / GVP

1960 eruption following the great Chile earthquake
Puyehue-Cordón Caulle Volcano started erupting on 24 May 1960. It is possible, that the eruption was triggered by the great earthquake in Chile (magnitude 9.5; the largest measured earthquake in history) on 22 May 1960. The eruption started with a powerful explosive (subplinian) phase, which formed an ash column 8 km high.

2011 eruption of Puyehue-Cordón Caulle
A new eruption started at the complex of Puyehue-Cordón Caulle volcano in Chile on Saturday 4 June 2011 after 51 years of inactivity.

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