🌋VolcanoAtlas

Sangay

Stratovolcano in Ecuador

Last Eruption: 2025

Key Facts

Elevation

5,286 m (17,343 ft)

Type

Stratovolcano

Location

-2.005°, -78.341°

Region

Northern Andean Volcanic Arc

Total Eruptions

11

Max VEI

VEI 3

Rock Type

Andesite / Basaltic Andesite

Tectonic Setting

Subduction zone

Location

Loading map...

Eruption Timeline

2025 CENotable

Most recent confirmed eruption

2020 CEVEI 3

Historical eruption (estimated)

2010 CEVEI 1

Historical eruption (estimated)

1985 CEVEI 3

Historical eruption (estimated)

1983 CEVEI 1

Historical eruption (estimated)

1971 CEVEI 1

Historical eruption (estimated)

1956 CEVEI 3

Historical eruption (estimated)

1949 CEVEI 1

Historical eruption (estimated)

1947 CEVEI 1

Historical eruption (estimated)

1940 CEVEI 3

Historical eruption (estimated)

1920 CEVEI 3

Historical eruption (estimated)

Overview

The isolated Sangay volcano, located east of the Andean crest, is the southernmost of Ecuador's volcanoes and its most active. The steep-sided, glacier-covered, dominantly andesitic volcano grew within the open calderas of two previous edifices which were destroyed by collapse to the east, producing large debris avalanches that reached the Amazonian lowlands. The modern edifice dates back to at least 14,000 years ago.

It towers above the tropical jungle on the east side; on the other sides flat plains of ash have been eroded by heavy rains into steep-walled canyons up to 600 m deep. The earliest report of an eruption was in 1628. Almost continuous eruptions were reported from 1728 until 1916, and again from 1934 to the present.

The almost constant activity has caused frequent changes to the morphology of the summit crater complex.

Volcanic Hazards & Risk Assessment

Primary Hazards

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

Risk Level

Population at RiskModerate
Infrastructure RiskHigh
Aviation RiskSignificant

Geological Composition & Structure

Rock Types

Primary
Andesite / Basaltic Andesite
Silica Content
Intermediate (57-63% SiO₂)

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 Eruptions11ModerateModerately active volcano
Maximum VEIVEI 3ModerateLocal impact potential
Recent Activity1 years agoVery RecentCurrently active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Active
Recent volcanic activity detected. Continuous monitoring in place.

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: 352090
  • Evidence: Eruption Observed
  • Epoch: Holocene

About the Photo

The isolated Sangay volcano towers above tropical jungles east of the Andean crest. Seen here from the NE, it is one of Ecuador's most active volcanoes and has been in frequent eruption during the past several centuries. The steep-sided, glacier-covered volcano has been constructed within the older Verdeloma somma to the south. Historical eruptions were first reported in 1628. More-or-less continuous eruptions took place from 1728 until 1916, and again from 1934 until the present.

Photo by Minard Hall, 1976 (Escuela Politécnica Nacional, Quito).

Basic Information

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