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Akan

Caldera in Japan

Last Eruption: 2025

Key Facts

Elevation

1,499 m (4,918 ft)

Type

Caldera

Location

43.384°, 144.013°

Region

Kuril Volcanic Arc

Total Eruptions

36

Max VEI

VEI 4

Rock Type

Andesite / Basaltic Andesite

Tectonic Setting

Subduction zone

Location

Loading map...

Eruption Timeline

2025 CEVEI 2Notable

Minor phreatic eruption at Meakandake

2018 CEVEI 1

Small phreatic eruption

2008 CEVEI 2

Phreatic eruptions from Ponmachineshiri crater

2006 CEVEI 1

Minor eruption at Meakandake

1998 CEVEI 1

Small phreatic activity

1996 CEVEI 2

Phreatomagmatic eruption

1988 CEVEI 2

Eruption at Meakandake with ashfall

1966 CEVEI 1

Minor activity

1964 CEVEI 1

Phreatic eruption

1962 CEVEI 1

Small eruption

1960 CEVEI 1

Minor phreatic activity

1959 CEVEI 1

Small eruption at crater

1958 CEVEI 1

Phreatic eruption

1957 CEVEI 1

Minor activity

1956 CEVEI 1

Small eruption

1955 CEVEI 2

Moderate eruption with ash emissions

1954 CEVEI 1

Minor phreatic eruption

1951 CEVEI 1

Small eruption

1874 CEVEI 2

Historical eruption

1808 CEVEI 2

Early 19th century activity

Overview

Akan is a 13 x 24 km caldera located immediately SW of Kussharo caldera in eastern Hokkaido. The elongated, irregular outline of the caldera rim reflects its incremental formation during major explosive eruptions from the early to mid-Pleistocene. There are four post-caldera stratovolcanoes, three at the SW end of the caldera and the other on the NE side.

Conical Oakandake was frequently active during the Holocene. The 1-km-wide Nakamachineshiri crater of Meakandake was formed during a major pumice-and-scoria eruption about 13,500 years ago. The Meakandake group, composed of nine overlapping cones E of Lake Akan, has produced mild phreatic eruptions since the beginning of the 19th century.

The main cone of Meakandake proper has a triple crater at its summit. Although recorded eruptions at Meakandake have consisted of minor phreatic explosions, four major magmatic eruptions with pyroclastic flows have also occurred during the Holocene.

Volcanic Hazards & Risk Assessment

Primary Hazards

  • Pyroclastic flows and surges
  • Large explosive eruptions (VEI 4+)
  • Ash fall and tephra deposits
  • Lahars and debris flows

Risk Level

Population at RiskHigh
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 Eruptions36HighHighly active volcano
Maximum VEIVEI 4MajorRegional impact potential
Recent Activity1 years agoVery RecentCurrently active

Monitoring & Alert Status

Monitoring Networks

Japan Meteorological Agency (JMA)
Real-time seismic monitoring
Geological Survey of Japan
Geochemical monitoring
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: 285070
  • Evidence: Eruption Observed
  • Epoch: Holocene

About the Photo

Oakandake, the largest post-caldera cone at Akan volcano, is seen here from the W across the Akan Caldera lake. It was constructed at the NE end of the 13 x 14 km caldera, opposite a cluster of stratovolcanoes at the SW end. Meakan in the SW group has been frequently active.

Photo by Wataru Hirose, 1996 (Hokkaido University).

Basic Information

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