Chile · Stratovolcano
Pular
- Type
- Stratovolcano
- Elevation
- 6233m
- Last eruption
- Unknown

- Type
- Stratovolcano
- Country
- Chile
- Region
- South America / Central Andean Volcanic Arc
- Elevation
- 6233m
- Coordinates
- -24.188, -68.054
- Last eruption
- Unknown
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic andesite
Geological summary
Cerro Pular on the NE end and Cerro Pajonales on the SW form a 12-km-long volcanic ridge NE of Socompa volcano that is mostly pre-Holocene, but may have experienced some more recent activity.
Excerpt from the Global Volcanism Program, Smithsonian Institution · Read the full summary on GVP →
From Wikipedia
Pular is a volcanic massif in the northern Chilean Andes, in the Antofagasta Region north of Socompa volcano. It consists of the individual mountains Pajonales and Pular, which are among the highest mountains in the region and of great cultural importance to the neighbouring towns of Socaire and Peine. Pular and Pajonales have multiple volcanic craters and have produced lava domes. The mountains were active during the last three million years; whether there was any activity in historical times is unclear. The mountains are largely unglaciated in the present, owing to the dry climate, although groundwater originates on them. During the Last Glacial Maximum, glacial advances left a girdle of moraines around the massif.
Wikipedia · CC BY-SA · Read full article →
Eruption history
1 recordedGlossaryRecord summary
- Confirmed eruptions
- 0
- Uncertain eruptions
- 1
Detailed timeline
- 1990VEI 1Method not stated1990-04-24 – 1990-04-24
Nearby volcanoes
External links
⚠ For reference only. Not for emergency response.