Putana
Stratovolcano · Chile · 5884m

- Type
- Stratovolcano
- Country
- Chile
- Region
- South America Volcanic Regions / Central Andean Volcanic Arc
- Elevation
- 5884m
- Coordinates
- -22.557, -67.853
- Last eruption
- 1810
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Dacite
Geological summary
Volcán Putana, also known as Jorgencal or Machuca, is part of a large, roughly N-S-trending volcanic complex that covers an area of 600 km2. Vigorous fumarolic activity is visible at the summit from long distances. The main edifice, which formed primarily by lava effusion, consists of accumulated postglacial dacitic lava domes and flows mantling an older pre-Holocene volcano. The youngest basaltic andesite lava flows are viscous and rarely extend more than 3 km. A major eruption of unspecified character was reported in the early 19th century (Rudolph, 1955; Guest 1981, pers. comm.), although González-Ferrán (1995) indicated that no historical eruptions had occurred.
From Wikipedia
Volcán Putana, sometimes referred to as Jorqencal or Machuca, is a stratovolcano located in the Central Volcanic Zone (CVZ) of the Andes on the border between Bolivia and Chile and close to the Sairecabur volcanic complex. Its summit is 5,884 metres (19,304 ft) above sea level and contains a summit crater with two smaller craters nested within it. Beneath the summit, the volcano features a number of lava domes and lava flows, some of which originated in flank vents.
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Eruption history
Detailed timeline
- 1972VEI ?Geological estimate1972-07-02 – Ongoing
- 1810 (±10 yrs)VEI ?Observed1810 – Ongoing
External links
⚠ For reference only. Not for emergency response.