File:Volcan_parinacota_1.JPG · Wikimedia Commons · See Wikimedia Commons
Key facts
- Elevation
- 6,380 m (20,930 ft)
- Listing
- Ultra
- Location
- Bolivia – Chile border
- Parent range
- Andes
- Mountain type
- Stratovolcano
- Volcanic zone
- Central Volcanic Zone
- Last eruption
- 290 CE ± 300 years
- Easiest route
- snow/rock scramble
via Wikipedia infobox
Wikidata facts
- Elevation
- 6348
- Image
- Parinacota.jpg
Show 4 more facts
- topographic isolation
- 20
- Commons category
- Parinacota
- topographic prominence
- 1150
- Commons gallery
- Parinacota
Sources (1)
via Wikidata · CC0
~40 min read
Article
Parinacota (in Hispanicized spelling), 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.
The volcano started growing during the Pleistocene and formed a large cone. At some point between the Pleistocene and the Holocene, the western flank of the volcano collapsed, generating a giant landslide that spread west and formed a large, hummocky landslide deposit. The avalanche crossed and dammed a previously existing drainage, impounding or enlarging Lake Chungará; numerous other lakes now forming the headwaters of the Rio Lauca sprang up within the deposit. Volcanic activity rebuilt the cone after the collapse, cancelling out the collapse scar.