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Huaynaputina

Stratovolcano in Peru

Last Eruption: 1600

Key Facts

Elevation

4,679 m (15,351 ft)

Type

Stratovolcano

Location

-16.614°, -70.854°

Region

Central Andean Volcanic Arc

Rock Type

Dacite

Tectonic Setting

Subduction zone

Location

Loading map...

Overview

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.

Volcanic Hazards & Risk Assessment

Primary Hazards

  • Pyroclastic flows
  • Lava flows
  • Volcanic bombs and ballistics
  • Lahars and mudflows

Risk Level

Population at RiskModerate
Infrastructure RiskModerate
Aviation RiskSignificant

Geological Composition & Structure

Rock Types

Primary
Dacite
Silica Content
Varied composition

Tectonic Setting

Subduction zone
Formed by oceanic plate subduction, typically producing explosive eruptions due to water-rich magmas.

Age & Formation

Epoch
Holocene
Evidence
Eruption Observed

Eruption Statistics & Analysis

MetricValueGlobal RankingSignificance
Total Recorded EruptionsUnknownLowModerately active volcano
Maximum VEIVEI UnknownMinorLocal impact potential
Recent Activity426 years agoHistoricalHistorically active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Normal
No recent activity. Routine monitoring continues.

Nearby Volcanoes in South America Volcanic Regions

Regional Volcanic Activity
The South America Volcanic Regions contains multiple active volcanic systems. Cross-regional magma interactions and tectonic stresses can influence eruption patterns across the entire arc. Monitor regional seismic activity and volcanic alerts.

Quick Info

  • Smithsonian ID: 354030
  • Evidence: Eruption Observed
  • Epoch: Holocene

About the Photo

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 by Oscar González-Ferrán (University of Chile).

Basic Information

This page shows basic data from the Smithsonian Global Volcanism Program. For more detailed information, visit the official Smithsonian page.