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Reclus

Pyroclastic cone in Chile

Last Eruption: 1908

Key Facts

Elevation

1,403 m (4,603 ft)

Type

Pyroclastic cone

Location

-50.940°, -73.580°

Region

Austral Andean Volcanic Arc

Rock Type

Dacite

Tectonic Setting

Subduction zone

Location

Loading map...

Overview

Reclus, the source of several Patagonian Holocene tephra layers, was recognized to be an independent volcanic edifice in 1987. The volcano consists of a large dacitic pyroclastic cone with a crater about 1 km in diameter. As many as six tephra layers overlie a peat layer dated at 3,780 years before present.

Research has also revealed evidence for eruptions in the 19th and early 20th centuries.

Volcanic Hazards & Risk Assessment

Primary Hazards

    Risk Level

    Population at RiskModerate
    Infrastructure RiskHigh
    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 Activity118 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: 358063
    • Evidence: Eruption Observed
    • Epoch: Holocene

    About the Photo

    Amalia Glacier flows around the northern flank of Reclus in the Southern Patagonia Ice Field, shown in this 27 February 2018 PlanetScope satellite image (N is at the top; this image is approximately 8 km across). The flanks are heavily eroded and there is a landslide deposit from the northern flank on the glacier surface.

    Satellite image courtesy of Planet Labs Inc., 2018 (https://www.planet.com/).

    Basic Information

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