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Diky Greben

Lava dome(s) in Russia

Last Eruption: 350

Key Facts

Elevation

1,040 m (3,412 ft)

Type

Lava dome(s)

Location

51.452°, 156.978°

Region

Kuril Volcanic Arc

Rock Type

Dacite

Tectonic Setting

Subduction zone

Location

Loading map...

Overview

Diky Greben is a lava-dome complex that formed in the center of the 20 x 25 km Pauzhetka caldera, which also contains the Kurile Lake caldera to the east. This large caldera was associated with eruption of the voluminous rhyolitic Golygin ignimbrite during the late Pleistocene, about 443,000 years ago. The initial Diky Greben eruptions took place about 7,600-7,700 years ago, immediately following the Kurile Lake eruption.

Most of the volcano, particularly the thick lava flows north and south of Nepriyatnaya Mountain, was formed during an eruption about 1,600 years ago. A total of 9-10 km3 of dacitic and 2-3 km3 of andesitic lavas and tephras were erupted at this time. Two large craters and a few smaller vents were formed after this eruption.

Volcanic Hazards & Risk Assessment

Primary Hazards

    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 Dated

    Eruption Statistics & Analysis

    MetricValueGlobal RankingSignificance
    Total Recorded EruptionsUnknownLowModerately active volcano
    Maximum VEIVEI UnknownMinorLocal impact potential
    Recent Activity1676 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 Northwestern Pacific Volcanic Regions

    Regional Volcanic Activity
    The Northwestern Pacific 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: 300022
    • Evidence: Eruption Dated
    • Epoch: Holocene

    About the Photo

    Diky Greben, seen here from the E along the Ozernaya River, is a Holocene lava dome complex that formed in the center of the 20 x 25 km Pleistocene Pauzhetka caldera. Early activity took place around 6,000 years ago. There are thick lava flows N and S of Nepriyatnaya dome (left-center horizon), which forms the summit of the complex.

    Photo by Oleg Dirksen, 1996 (Institute of Volcanology, Petropavlovsk).

    Basic Information

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