Volcano profile · Aleutian Islands, Alaska

Great
Sitkin

A remote Aleutian volcano known for slow crater-filling lava, difficult weather and monitoring that often depends on satellites and instruments.

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Great Sitkin can change gradually or with little visual warning. View the Volcoholics volcano directory for the latest verified official position from the Alaska Volcano Observatory.

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A remote Aleutian eruption

Slow lava, deep snow and a watchful sky

Great Sitkin rises from a small island in the central Aleutians, more than 40 kilometres east of Adak.

The present eruption began with an explosion in May 2021, followed by slow lava effusion from July that year. Since then, lava has filled most of the summit crater, overridden older domes and advanced into valleys outside the crater.

Unlike the explosive ash crises associated with many Aleutian volcanoes, Great Sitkin's recent behaviour is primarily effusive. Its remoteness makes satellites, local instruments and aviation monitoring especially important.

1,740 mElevation
WATCHVolcano alert level
ORANGEAviation colour code
2021–presentRecent eruptive period
Great Sitkin volcano and the surrounding Aleutian landscape
Credit: Image courtesy of Steve Rhodes. (AVO)
Great Sitkin quick facts
Volcano type
Stratovolcano
Location
Andreanof Islands, Alaska
Characteristic style
Slow summit lava effusion
Nearest community
Adak
Official agency
Alaska Volcano Observatory
Activity and behaviour

Slow lava growth inside a remote crater

Evergreen profile
How Great Sitkin behaves

Great Sitkin is known for prolonged episodes of slow lava effusion, crater-filling dome growth and low-level seismicity. Cloud, snow and darkness often obscure the summit, so satellites and instruments are essential.

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Typical recent styleSlow lava effusionCrater-filling growth can persist for years
VisibilityFrequently obscuredCloud, snow and darkness limit direct observation
SeismicityOften low levelSmall earthquakes and rockfall signals may occur
Main toolsSatellite and seismicRemote sensing is central to monitoring
Official sourceAVO / USGSAuthoritative alert and aviation information
US volcano alert system

What WATCH and ORANGE mean

WATCH indicates heightened or escalating unrest or an eruption with limited hazards. ORANGE means an eruption is underway or likely, but ash emissions are absent or minor at aviation altitudes.

Normal / GreenBackground activity

No eruption and typical monitoring levels.

Advisory / YellowElevated unrest

Activity is above background but hazards remain limited.

Watch / OrangeEruption underway

Great Sitkin's current slow lava eruption fits this operational category.

Warning / RedMajor hazardous eruption

Significant ash emissions or severe ground hazards are underway or imminent.

Inside the summit crater

A volcano rewriting its own crater

Great Sitkin's eruption is slow enough to reveal each stage of lava emplacement.

Fresh lava emerges inside the 2021 explosion crater, thickens across the crater floor and gradually pushes outward. The eruption has transformed the summit without the sustained ash production seen in many Aleutian crises.

Summit ventFresh lava rises inside the 2021 explosion crater.
Crater fillingThick lava spreads across older summit deposits.
Rim crossingActive lobes move beyond the crater edge.
Slow advanceFlow fronts creep east–southeast with minor rockfalls.
Simplified Great Sitkin summit crater and lava-flow growth
Great Sitkin's summit lava system, simplified and not to scale.
How Great Sitkin is erupting

From crater explosion to years of slow lava

01May 2021 explosionAn ash-and-gas plume opened the current crater.
02Lava beginsEffusion was established by July 2021.
03Crater fillsLava spreads across older summit domes.
04Flow overflowsActive lobes advance beyond the crater.
05Slow expansionThermal anomalies and minor rockfalls continue.
Illustrative Great Sitkin monitoring network
Monitoring

Monitoring Great Sitkin

Through cloud, snow and darkness

AVO combines local instruments with satellite radar and thermal imagery because Aleutian weather often hides the summit from direct view.

Seismic networkTracks earthquakes, rockfalls and changes in eruptive activity.
InfrasoundDetects explosive pressure waves locally and regionally.
Satellite radarMaps lava growth even through cloud and darkness.
Thermal imageryIdentifies active, snow-free areas on the dome and flows.
WebcamsProvide visual confirmation when Aleutian weather allows.
Lightning networksHelp detect ash-rich explosive activity across the region.
Why Great Sitkin matters

A natural laboratory for slow lava emplacement

Great Sitkin gives scientists an unusually long view of how lava spreads, thickens and advances inside a summit crater. Because the eruption evolves gradually, satellite radar, thermal imagery, seismic instruments and remote cameras can measure subtle changes over months and years rather than minutes.

That slow pace allows AVO to compare radar scenes across weeks and seasons, tracking flow-front movement, crater filling and snow-free thermal areas in a way that would be impossible during a short, fast-moving eruption.

A volcano through time

Great Sitkin eruption timeline

1945

Wartime-era eruption

Explosive and lava-dome activity left deposits later overridden by the recent eruptive period.

1974

Short explosive eruption

Ash emission and dome activity created another important layer in the summit crater.

Recent eruptive period begins25 May 2021

Explosion opens the new eruptive phase

An explosion sent ash and gas to roughly 4.6 kilometres above sea level, after which activity shifted toward long-lived lava effusion.

Explosion → effusion Within weeks, Great Sitkin changed from an explosive eruption to one of the world's clearest modern examples of long-lived crater-filling lava effusion.
Jul–Aug 2021

Lava fills and overflows the crater

Fresh lava spread over the 1945 and 1974 domes, overrode summit ice and moved beyond the crater rim.

2022–25

Persistent slow effusion

The crater-filling lava field expanded gradually, with intermittent thermal anomalies and rockfalls.

Current phase2026

East–southeast lava growth continues

Satellite radar confirms continued expansion while seismicity remains low and no new explosions have occurred.

What matters most

Great Sitkin's main hazards

Aviation ash

A renewed explosion could inject ash into busy central Aleutian air routes.

Lava flows and rockfalls

Slow lava can destabilise steep margins and send blocks down summit valleys.

Snow and ice interaction

Hot lava over snow and ice creates steam, meltwater and unstable ground.

Aviation disruption

Remote air routes require rapid detection of any ash-producing change.

Volcoholics InsightGreat Sitkin demonstrates that an eruption can remain significant even when it is slow, quiet and almost entirely hidden by Aleutian weather.
Myths and reality

Great Sitkin myths, separated from the science

Myth

No explosions means the eruption is over.

Reality: lava has continued to erupt slowly since 2021 despite the absence of new explosions.

Myth

Low seismicity means no magma is moving.

Reality: slow effusion can continue with only weak earthquake and rockfall signals.

Myth

Cloud cover means the volcano cannot be monitored.

Reality: satellite radar can map lava growth through cloud and darkness.

Myth

A remote volcano creates little risk.

Reality: ash-producing changes could affect aviation even when few people live nearby.

Volcoholics Insight

An eruption measured in years, not minutes

Great Sitkin is the opposite of a brief volcanic spectacle. Its present eruption is a slow transformation of the summit crater, documented through thermal pixels, radar images and small rockfall signals across a remote island landscape.

Questions answered

Great Sitkin explained

What type of activity is Great Sitkin known for?

Great Sitkin is known for prolonged slow lava effusion, crater-filling dome growth and low-level seismicity. The intensity and visibility of activity vary over time.

When did the recent eruptive period begin?

An explosion occurred on 25 May 2021, followed by sustained lava effusion beginning in July 2021.

Why is the aviation colour code Orange?

An eruption is underway, although the current phase is primarily effusive and has not produced significant ash since May 2021.

How can AVO monitor through cloud?

Satellite radar, thermal data, seismic instruments and infrasound continue working when visual observations are limited.

Where is Great Sitkin?

On Great Sitkin Island in Alaska's Andreanof Islands, east of the community of Adak.

Official science, made readable

Built from the agencies watching Great Sitkin

Operational status belongs to the Alaska Volcano Observatory and USGS. Volcoholics provides context and never replaces official aviation or hazard notices.

Alaska Volcano ObservatoryUSGSAlaska Division of Geological & Geophysical SurveysNOAA