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McDonald Islands

Complex in Australia

Last Eruption: 2005

Key Facts

Elevation

263 m (863 ft)

Type

Complex

Location

-53.039°, 72.595°

Region

Kerguelen Hotspot Volcano Group

Rock Type

Phonolite

Tectonic Setting

Intraplate

Location

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Overview

The McDonald Islands are located on the Kerguelen Plateau about 75 km W of Heard Island. The largest island, McDonald, is composed of a layered phonolitic tuff plateau cut by phonolitic dikes and lava domes. A possible nearby active submarine center was inferred from phonolitic pumice that washed up on Heard Island in 1992.

Volcanic plumes were observed in December 1996 and January 1997 from McDonald Island. During March 1997 the crew of a vessel that sailed near the island noted vigorous steaming from a vent on the N side of the island along with possible pyroclastic deposits and lava flows. A satellite image taken in November 2001 showed the island to have more than doubled in area since previous reported observations in November 2000.

Volcanic Hazards & Risk Assessment

Primary Hazards

    Risk Level

    Population at RiskModerate
    Infrastructure RiskHigh
    Aviation RiskSignificant

    Geological Composition & Structure

    Rock Types

    Primary
    Phonolite
    Silica Content
    Varied composition

    Tectonic Setting

    Intraplate
    Continental rift or intraplate setting with varied eruptive styles.

    Age & Formation

    Epoch
    Holocene
    Evidence
    Eruption Observed

    Eruption Statistics & Analysis

    MetricValueGlobal RankingSignificance
    Total Recorded EruptionsUnknownLowModerately active volcano
    Maximum VEIVEI UnknownMinorLocal impact potential
    Recent Activity21 years agoRecentRecently active

    Monitoring & Alert Status

    Monitoring Networks

    Global Volcanism Program
    International eruption database

    Current Status

    Watch
    Dormant but monitored. Capable of renewed activity.

    Nearby Volcanoes in Somalian-Antarctic Volcanic Regions

    Regional Volcanic Activity
    The Somalian-Antarctic 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: 234011
    • Evidence: Eruption Observed
    • Epoch: Holocene

    About the Photo

    Three small, low islands on the Kerguelen Plateau form the McDonald Islands. The largest island, McDonald, is only 1 km2 in area and around 200 m high. This April 1997 photo shows a plume at Samarang Hill (right). The Island is composed of a layered tuff plateau cut by dikes and lava domes. A possible nearby active submarine center was inferred from pumice that washed up on Heard Island in 1992. The snow-capped peak in the background is Heard volcano, 44 km to the E.

    Copyrighted photo by Richard Williams, 1997 (Australian Antarctic Div., published in Global Volcanism Network Bulletin).

    Basic Information

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