Skip to main content

Huaynaputina

Stratovolcano · Peru · 4679m

Huaynaputina is a relatively inconspicuous volcano that was the source of one of the largest historical eruptions of the central Andes in 1600 CE.  The volcano has no prominent topographic expression.  This view is from the east into a 2.5-km-wide complex caldera that is breached widely to the east.  Three ash cones, one of which can be seen in the shadow at the right-center, are located on the floor of the caldera.  Light-colored ash deposits from the 1600 eruption can be seen mantling the caldera rim.
Huaynaputina is a relatively inconspicuous volcano that was the source of one of the largest historical eruptions of the central Andes in 1600 CE. The volcano has no prominent topographic expression. This view is from the east into a 2.5-km-wide complex caldera that is breached widely to the east. Three ash cones, one of which can be seen in the shadow at the right-center, are located on the floor of the caldera. Light-colored ash deposits from the 1600 eruption can be seen mantling the caldera rim. · Photo: Photo by Oscar González-Ferrán (University of Chile).
Type
Stratovolcano
Country
Peru
Region
South America Volcanic Regions / Central Andean Volcanic Arc
Elevation
4679m
Coordinates
-16.614, -70.854
Last eruption
1600
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Dacite
Geological summary

Huaynaputina (whose name means "new volcano") was the source of the largest historical eruption of South America in 1600 CE. It has no prominent topographic expression and lies within a 2.5-km-wide collapse depression and further excavated by glaciers within a Tertiary to Pleistocene edifice. Three overlapping ash cones with craters up to 100 m deep were constructed during the 1600 CE eruption on the floor of the older crater, whose outer flanks are heavily mantled by ash deposits from the 1600 eruption. This powerful fissure-fed eruption may have produced nearly 30 km3 of dacitic tephra, including pyroclastic flows and surges that traveled 13 km to the E and SE. Lahars reached the Pacific Ocean, 120 km away. The eruption caused substantial damage to the major cities of Arequipa and Moquengua.

From Wikipedia

Huaynaputina is a volcano in a volcanic high plateau in southern Peru. Lying in the Central Volcanic Zone of the Andes, it was formed by the subduction of the oceanic Nazca Plate under the continental South American Plate. Huaynaputina is a large volcanic crater, which lacks an identifiable mountain profile, with an outer stratovolcano and three younger volcanic vents within an amphitheatre-shaped structure that is either a former caldera or a remnant of glacial erosion. The volcano has erupted dacitic magma.

Wikipedia · CC BY-SA · Read full article

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
7750 BCE~7438 BCE · 1 eruptions · max VEI ?1288~1600 · 1 eruptions · max VEI 67750 BCE5568 BCE3075 BCE893 BCE1288

Detailed timeline

  1. 1600VEI 6Observed
    1600-02-17 – 1600-03-06
    Summit and south flank
  2. 7750 BCE (±200 yrs)VEI ?Geological estimate
    BCE 7750 – Ongoing

External links

⚠ For reference only. Not for emergency response.