Chiles-Cerro Negro
Stratovolcano · Colombia-Ecuador · 4698m
- Type
- Stratovolcano
- Country
- Colombia-Ecuador
- Region
- South America Volcanic Regions / Northern Andean Volcanic Arc
- Elevation
- 4698m
- Coordinates
- 0.817, -77.938
- Last eruption
- 1936
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Dacite
Geological summary
The Chiles-Cerro Negro volcanic complex includes both the Pleistocene Chiles and the Cerro Negro de Mayasquer stratovolcanoes astride the Colombia-Ecuador border. Cerro Negro has a caldera open to the west, with andesitic and dacitic lava flows of possible Holocene age (Hall 1992, pers. comm.) and solfataras on the shore of a small crater lake. An eruption reported in 1936 may have been from Reventador (Catalog of Active Volcanoes of the World). The higher, glacier-covered summit of Chiles, about 4 km ESE of Cerro Negro, last erupted about 160,000 years ago, but it has a caldera open to the north with hot springs and an active hydrothermal system on its eastern flank.
From Wikipedia
Cerro Negro de Mayasquer is a volcano on the border of Colombia and Ecuador. It lies 3 kilometres (2 mi) north-west of the volcano Chiles, and the two peaks are considered part of the same Chiles-Cerro Negro volcanic complex. These volcanoes, together with Cumbal are andesitic in rock type. A 1936 eruption reported by the Colombian government agency INGEOMINAS may have been from the Ecuadorean volcano Reventador, otherwise the volcano has not erupted for around 160,000 years.
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Eruption history
Detailed timeline
- 1936VEI 2Observed1936-07-17 – OngoingVolcano Uncertain: possibly Reventador
External links
⚠ For reference only. Not for emergency response.