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Sarychev Peak

Stratovolcano in Russia

Last Eruption: 2021

Key Facts

Elevation

1,496 m (4,908 ft)

Type

Stratovolcano

Location

48.092°, 153.200°

Region

Kuril Volcanic Arc

Total Eruptions

20

Max VEI

VEI 4

Rock Type

Andesite / Basaltic Andesite

Tectonic Setting

Subduction zone

Location

Loading map...

Eruption Timeline

2021 CENotable

Most recent confirmed eruption

2014 CEVEI 3

Historical eruption (estimated)

2002 CEVEI 2

Historical eruption (estimated)

1992 CEVEI 1

Historical eruption (estimated)

1989 CEVEI 2

Historical eruption (estimated)

1986 CEVEI 1

Historical eruption (estimated)

1971 CEVEI 1

Historical eruption (estimated)

1946 CEVEI 1

Historical eruption (estimated)

1916 CEVEI 1

Historical eruption (estimated)

1896 CEVEI 2

Historical eruption (estimated)

1886 CEVEI 2

Historical eruption (estimated)

1874 CEVEI 3

Historical eruption (estimated)

1862 CEVEI 2

Historical eruption (estimated)

1855 CEVEI 2

Historical eruption (estimated)

1830 CEVEI 2

Historical eruption (estimated)

1805 CEVEI 1

Historical eruption (estimated)

Overview

Sarychev Peak, one of the most active volcanoes of the Kuril Islands, occupies the NW end of Matua Island in the central Kuriles. The andesitic central cone was constructed within a 3-3. 5-km-wide caldera, whose rim is exposed only on the SW side.

A dramatic 250-m-wide, very steep-walled crater with a jagged rim caps the volcano. The substantially higher SE rim forms the 1496 m high point of the island. Fresh-looking lava flows, prior to activity in 2009, had descended in all directions, often forming capes along the coast.

Much of the lower-angle outer flanks of the volcano are overlain by pyroclastic-flow deposits. Eruptions have been recorded since the 1760s and include both quiet lava effusion and violent explosions. Large eruptions in 1946 and 2009 produced pyroclastic flows that reached the sea.

Volcanic Hazards & Risk Assessment

Primary Hazards

  • Pyroclastic flows
  • Lava flows
  • Volcanic bombs and ballistics
  • Lahars and mudflows

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 Eruptions20ModerateModerately active volcano
Maximum VEIVEI 4MajorRegional impact potential
Recent Activity5 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 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: 290240
  • Evidence: Eruption Observed
  • Epoch: Holocene

About the Photo

One of the largest recorded eruptions in the Kuril Islands took place 11-16 June from Sarychev Peak. This NASA Space Shuttle view on 12 June shows an eruption plume that rose to 16-21 km altitude; pyroclastic flows reached the sea and extended the shoreline in some areas. The main explosive phase ended on 16 June, but weak explosions producing ash plumes continued prior to arrival of a field team on 26-28 July, when no eruptive activity was observed.

NASA International Space Station image ISS020-E-9048, 2009 (http://eol.jsc.nasa.gov/).

Basic Information

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