Purupuruni
Sign in to savePurupuruni is a group of lava domes in southern Peru and a correlative geological formation. They are among the many volcanoes that exist in Peru and whose activity has been associated with the subduction of the Nazca Plate beneath the South America Plate. Purupuruni is associated with a geothermal field and a caldera. Volcanic activity occurred during the Pleistocene 53,000 ± 8,000 years ago but also during the Holocene about 5,300 ± 1,100 years ago; today the volcano is considered to be a low hazard volcano but is being monitored nevertheless.
In the Vinony graph
Vinony's link graph records 167 inbound references to Purupuruni, and connects out to Misti, Chile and Peru.
The entry is geolocated on the map in mountain_region, across 2 mapped points.
Vinony files it under Five-thousanders of the Andes, Holocene volcanoes and Mountains of the Department of Tacna.
Vinony links it to 5 Wikipedia language editions.
Wikidata facts
- Instance of
- lava dome
- Country
- Peru
- Located in
- Tacna Department
- Elevation
- 5315
Show 1 more fact
- mountain range
- Andes
via Wikidata · CC0
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Encyclopedic overview
6 sectionsContents
- Geography and geomorphology
- Geology
- Geological context
- Geologic history
- References
- Sources
Purupuruni is a group of lava domes in southern Peru and a correlative geological formation. They are among the many volcanoes that exist in Peru and whose activity has been associated with the subduction of the Nazca Plate beneath the South America Plate. Purupuruni is associated with a geothermal field and a caldera. Volcanic activity occurred during the Pleistocene 53,000 ± 8,000 years ago but also during the Holocene about 5,300 ± 1,100 years ago; today the volcano is considered to be a low hazard volcano but is being monitored nevertheless.
== Geography and geomorphology ==
Excerpted from Wikipedia’s “Purupuruni” article, available under the CC BY-SA 4.0 licence.
On the map
2 mapped locations