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Dempo

Stratovolcano(es) in Indonesia

Last Eruption: 2025

Key Facts

Elevation

3,142 m (10,308 ft)

Type

Stratovolcano(es)

Location

-4.016°, 103.121°

Region

Sunda Volcanic Arc

Total Eruptions

33

Max VEI

VEI 2

Rock Type

Andesite / Basaltic Andesite

Tectonic Setting

Subduction zone

Location

Loading map...

Eruption Timeline

2025 CENotable

Most recent confirmed eruption

2022 CEVEI 2

Historical eruption (estimated)

2002 CEVEI 2

Historical eruption (estimated)

1992 CEVEI 3

Historical eruption (estimated)

1982 CEVEI 1

Historical eruption (estimated)

1970 CEVEI 1

Historical eruption (estimated)

1965 CEVEI 1

Historical eruption (estimated)

1950 CEVEI 2

Historical eruption (estimated)

1940 CEVEI 2

Historical eruption (estimated)

1933 CEVEI 2

Historical eruption (estimated)

1903 CEVEI 3

Historical eruption (estimated)

1888 CEVEI 1

Historical eruption (estimated)

1863 CEVEI 3

Historical eruption (estimated)

1843 CEVEI 3

Historical eruption (estimated)

1823 CEVEI 3

Historical eruption (estimated)

1811 CEVEI 1

Historical eruption (estimated)

Overview

Dempo is a stratovolcano that rises above the Pasumah Plain of SE Sumatra. The andesitic complex has two main peaks, Gunung Dempo and Gunung Marapi, constructed near the SE rim of a 3-km-wide amphitheater open to the north. The high point of the older Gunung Dempo crater rim is slightly lower, and lies at the SE end of the summit complex.

The taller Marapi cone was constructed within the older crater. Remnants of seven craters are found at or near the summit, with volcanism migrating WNW over time. The active 750 x 1,100 m active crater cuts the NW side of the Marapi cone and contains a 400-m-wide lake at the far NW end.

Eruptions recorded since 1817 have been small-to-moderate explosions that produced local ashfall.

Volcanic Hazards & Risk Assessment

Primary Hazards

    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 Eruptions33HighHighly active volcano
    Maximum VEIVEI 2MinorLocal 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 Sunda-Banda Volcanic Regions

    Regional Volcanic Activity
    The Sunda-Banda 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: 261230
    • Evidence: Eruption Observed
    • Epoch: Holocene

    About the Photo

    The youngest crater of Dempo volcano, at the WNW end of a series of six partially overlapping craters at the summit, contains a 400-m-wide crater lake that has been the source of frequent phreatic eruptions during historical time. A seventh smaller crater is located on the upper N flank. Dempo is one of Sumatra's most active volcanoes, frequently producing small-to-moderate explosive eruptions.

    Photo by Ruska Hadian, 1989 (Volcanological Survey of Indonesia).

    Basic Information

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