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Sedanka Lava Field

Volcanic field in Russia

Last Eruption: -7050

Key Facts

Elevation

1,399 m (4,590 ft)

Type

Volcanic field

Location

57.317°, 160.067°

Region

Central Kamchatka Volcanic Arc

Rock Type

Basalt / Picro-Basalt

Tectonic Setting

Subduction zone

Location

Loading map...

Overview

The Sedanka lava field (Sedanka Dol) is located immediately west of the Sredinny Range axis and is formed by dominantly mafic lavas from small strato- and shield-like volcanoes, along with more than 100 cinder and lava cones of the late Pleistocene-Holocene age. For this compilation the volcanic field area is considered to be up to 10 km wide and stretching about 25 km from south of Gorny Institute volcano towards the NNW between Tuzovsky volcano to the SW and Titila to the NE. Other workers (eg.

Nekrylov et al. , 2015) define the field to include the eight large edifices from Terpuk on the SW to Shishel on the NE.

Volcanic Hazards & Risk Assessment

Primary Hazards

    Risk Level

    Population at RiskModerate
    Infrastructure RiskModerate
    Aviation RiskSignificant

    Geological Composition & Structure

    Rock Types

    Primary
    Basalt / Picro-Basalt
    Silica Content
    Low (45-52% 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 Dated

    Eruption Statistics & Analysis

    MetricValueGlobal RankingSignificance
    Total Recorded EruptionsUnknownLowModerately active volcano
    Maximum VEIVEI UnknownMinorLocal impact potential
    Recent Activity9076 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: 300520
    • Evidence: Eruption Dated
    • Epoch: Holocene

    About the Photo

    Several scoria cones on the Sedanka Lava Field are shown in this September 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 13 km across). The Gorny Institute volcanic complex is to the upper right and the Sredny scoria cone of Tuzovsky is to the upper left, and between them are scoria cones of Sedanka. The field has more than 100 cones across an area of around 10 km.

    Satellite image courtesy of Planet Labs Inc., 2019 (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.