Chile · Stratovolcano
Cordón Caulle
Puyehue-Cordon Caulle
- Type
- Stratovolcano
- Elevation
- 2236m
- Last eruption
- 2012

- Type
- Stratovolcano
- Country
- Chile
- Region
- South America / Southern Andean Volcanic Arc
- Elevation
- 2236m
- Coordinates
- -40.590, -72.117
- Last eruption
- 2012
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic andesite
Geological summary
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 volcano was constructed above a 5-km-wide caldera and is capped by a 2.4-km-wide Holocene summit caldera. Lava flows and domes of mostly rhyolitic composition are found on the E flank. 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. The Cordón Caulle geothermal area, occupying a 6 x 13 km wide volcano-tectonic depression, is the largest active geothermal area of the southern Andes volcanic zone.
From Wikipedia
Puyehue and Cordón Caulle are two coalesced volcanic edifices that form a major mountain massif in Puyehue National Park in the Andes of Ranco Province, in the South of Chile. In volcanology this group is known as the Puyehue-Cordón Caulle Volcanic Complex (PCCVC). Four volcanoes constitute the volcanic group or complex, the Cordillera Nevada caldera, the Pliocene Mencheca volcano, Cordón Caulle fissure vents and the Puyehue stratovolcano.
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Eruption history
26 recordedGlossaryDetailed timeline
- 2011VEI 5Observed2011-06-04 – 2012-04-21Cordón Caulle, N of the 1960 eruption fissure
- 1990VEI 1Observed1990-07-02 – end unknownCordón Caulle
- 1960VEI 3Observed1960-05-24 – 1960-07-30Cordón Caulle
- 1934VEI 2Observed1934-03-06 – end unknownCordón Caulle
- 1929VEI 2Observed1929-01-07 – end unknownCordón Caulle
- 1921VEI 3Observed1921-12-13 – 1922-02-12Cordón Caulle-Cordillera Nevada
- 1919VEI 2Observed1919-07-02 – 1920-07-02Cordón Caulle
- 1914VEI 2Observed1914-02-08 – end unknownCordón Caulle
- 1905VEI 2Observed1905-07-02 – end unknownCordón Caulle
- 1893VEI 2Observed1893-07-02 – end unknownCordón Caulle
- 1759VEI 2Observed1759 – end unknownCordón Caulle
- 1220 (±150 yrs)VEI ?Geological estimate1220 – end unknown
- 1140 (±100 yrs)VEI ?Geological estimate1140 – end unknown
- 860 (±75 yrs)VEI 5Geological estimate860 – end unknownPuyehue
- 500 (±100 yrs)VEI ?Geological estimate500 – end unknown
- 140 (±300 yrs)VEI ?Geological estimate140 – end unknownPuyehue?
- 110 (±200 yrs)VEI ?Geological estimate110 – end unknown
- 490 BCE (±300 yrs)VEI ?Geological estimate490 BCE – end unknown
- 990 BCE (±500 yrs)VEI ?Geological estimate990 BCE – end unknown
- 1490 BCE (±150 yrs)VEI ?Geological estimate1490 BCE – end unknown
- 3250 BCE (±2400 yrs)VEI ?Geological estimate3250 BCE – end unknownPuyehue
- 4230 BCE (±200 yrs)VEI ?Geological estimate4230 BCE – end unknown
- 4450 BCE (±900 yrs)VEI ?Geological estimate4450 BCE – end unknownPuyehue
- 4460 BCEVEI ?Geological estimate4460 BCE – end unknown
- 4690 BCE (±200 yrs)VEI ?Geological estimate4690 BCE – end unknown
- 5080 BCE (±150 yrs)VEI 5Geological estimate5080 BCE – end unknownPuyehue
Nearby volcanoes
External links
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