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Parinacota

Stratovolcano · Chile-Bolivia · 6336m

Glacier-clad Volcán Parinacota rises to the NE above Laguna Chungará near the Chile-Bolivia border.  The lake was formed when collapse of Parinacota about 8000 years ago produced a 6 cu km debris avalanche that traveled 22 km to the west and blocked drainages.  Subsequent eruptions constructed the 6348-m-high symmetrical stratovolcano, which towers above late-Pleistocene andesitic-to-rhyolitic lava domes and flows in the middle ground.
Glacier-clad Volcán Parinacota rises to the NE above Laguna Chungará near the Chile-Bolivia border. The lake was formed when collapse of Parinacota about 8000 years ago produced a 6 cu km debris avalanche that traveled 22 km to the west and blocked drainages. Subsequent eruptions constructed the 6348-m-high symmetrical stratovolcano, which towers above late-Pleistocene andesitic-to-rhyolitic lava domes and flows in the middle ground. · Photo: Photo by Lee Siebert, 2004 (Smithsonian Institution). · Wikimedia Commons
Type
Stratovolcano
Country
Chile-Bolivia
Region
South America Volcanic Regions / Central Andean Volcanic Arc
Elevation
6336m
Coordinates
-18.166, -69.142
Last eruption
290
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Andesite / Basaltic Andesite
Geological summary

The symmetrical Volcán Parinacota is the southernmost and youngest of a pair of volcanoes forming the Nevados de Payachata group along the Chile-Bolivia border. The dominantly Pleistocene Pomerape volcano towers above a low saddle to the NE. Collapse of Parinacota about 8,000 years ago produced a 6 km3 debris avalanche that traveled 22 km W and blocked drainages, forming Lake Chungará. Holocene eruptive activity has subsequently reconstructed the stratovolcano, which contains a pristine, 300-m-wide summit crater and youthful lava flows on the W flanks. Although no historical eruptions are known, Helium surface-exposure dates have been obtained for eruptions during the past two thousand years both from the main cone and the Ajata group of satellite cones and lava flows on the S and SW flanks.

From Wikipedia

Parinacota, Parina Quta or Parinaquta is a dormant stratovolcano on the border of Bolivia and Chile. Together with Pomerape it forms the Nevados de Payachata volcanic chain. Part of the Central Volcanic Zone of the Andes, its summit reaches an elevation of 6,380 metres (20,930 ft) above sea level. The symmetrical cone is capped by a summit crater with widths of 1 kilometre (0.62 mi) or 1,000 metres (3,300 ft). Farther down on the southern slopes lie three parasitic centres known as the Ajata cones. These cones have generated lava flows. The volcano overlies a platform formed by lava domes and andesitic lava flows.

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Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
7950 BCE~7675 BCE · 1 eruptions · max VEI ?6027 BCE~5753 BCE · 1 eruptions · max VEI ?4379 BCE~4105 BCE · 1 eruptions · max VEI ?1358 BCE~1083 BCE · 1 eruptions · max VEI ?15~290 · 2 eruptions · max VEI 47950 BCE6027 BCE3830 BCE1907 BCE15

Detailed timeline

  1. 290 (±300 yrs)VEI 4Geological estimate
    290 – Ongoing
    Parinacota 3 edifice
  2. 90 (±50 yrs)VEI ?Geological estimate
    90 – Ongoing
    South flank (upper Volcanes de Ajata)
  3. 1100 BCE (±500 yrs)VEI ?Geological estimate
    BCE 1100 – Ongoing
    South flank (lower Volcanes de Ajata)
  4. 4320 BCE (±1200 yrs)VEI ?Geological estimate
    BCE 4320 – Ongoing
    South flank (lower Volcanes de Ajata)
  5. 5840 BCE (±50 yrs)VEI ?Geological estimate
    BCE 5840 – Ongoing
  6. 7950 BCEVEI ?Geological estimate
    BCE 7950 – Ongoing
    Ajata

External links

⚠ For reference only. Not for emergency response.