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Corcovado Volcano

Corcovado

Stratovolcano · Chile · 1826m

The dramatic summit spire of Volcán Corcovado is seen here in an aerial view from the south. Two of a string of lakes on its eastern side appear in the background. Corcovado, probably of late-Pleistocene age, is eroded by glaciers and surrounded by Holocene cinder cones. Eruptions were reported in historical time from these flank cones. Darwin observed activity from the Corcovado area in 1834, and an eruption was reported to have occurred in November 1835.
The dramatic summit spire of Volcán Corcovado is seen here in an aerial view from the south. Two of a string of lakes on its eastern side appear in the background. Corcovado, probably of late-Pleistocene age, is eroded by glaciers and surrounded by Holocene cinder cones. Eruptions were reported in historical time from these flank cones. Darwin observed activity from the Corcovado area in 1834, and an eruption was reported to have occurred in November 1835. · Photo: Photo by Oscar González-Ferrán (University of Chile). · Wikimedia Commons
Type
Stratovolcano
Country
Chile
Region
South America Volcanic Regions / Southern Andean Volcanic Arc
Elevation
1826m
Coordinates
-43.189, -72.794
Last eruption
-4920
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Andesite / Basaltic Andesite
Geological summary

Little is known of this isolated volcano that was seen in eruption by Darwin in 1834, and an eruption was reported to have occurred in November 1835. Corcovado, probably of late-Pleistocene age, is eroded by glaciers and surrounded by Holocene cinder cones. A series of lakes flank the eastern side of the basaltic to basaltic andesite structure. Eruptions in historical time were considered likely from these postglacial volcanoes (Moreno 1985, pers. comm.).

From Wikipedia

Corcovado Volcano is a stratovolcano located about 25 kilometres (16 mi) south of the mouth of the Yelcho River, in the Palena Province, Los Lagos Region, Chile. The glacially eroded volcano is flanked by Holocene cinder cones. The volcano's base has likely prehistoric lava flows that are densely vegetated. The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano. At its foot lies a series of lakes. Corcovado dominates the landscape of the Gulf of Corcovado area and is visible from Chiloé Island, weather permitting.

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Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
6640 BCE~6357 BCE · 1 eruptions · max VEI ?6075 BCE~5792 BCE · 1 eruptions · max VEI ?4945 BCE~4662 BCE · 1 eruptions · max VEI ?1553~1835 · 2 eruptions · max VEI 26640 BCE4662 BCE2402 BCE425 BCE1553

Detailed timeline

  1. 1835VEI 2Geological estimate
    1835-11-11 – Ongoing
  2. 1834VEI 2Geological estimate
    1834-11 – Ongoing
  3. 4920 BCE (±100 yrs)VEI ?Geological estimate
    BCE 4920 – Ongoing
  4. 6030 BCE (±100 yrs)VEI ?Geological estimate
    BCE 6030 – Ongoing
  5. 6640 BCE (±770 yrs)VEI ?Geological estimate
    BCE 6640 – Ongoing

External links

⚠ For reference only. Not for emergency response.