🌋VolcanoAtlas

Reykjanes

Iceland's Reawakened Volcanic Frontier

Elevation

140 m

Last Eruption

2025

Type

Crater rows / Fissure system

Country

Iceland

Location

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Volcanic Hazards & Risk Assessment

Primary Hazards

  • Lava flows and fountaining
  • Volcanic gas emissions
  • Local explosive activity

Risk Level

Population at RiskHigh
Infrastructure RiskHigh
Aviation RiskSignificant

Geological Composition & Structure

Rock Types

Primary
Unknown
Silica Content
Varied composition

Tectonic Setting

Unknown
Intraplate setting with hotspot or regional volcanic activity.

Age & Formation

Epoch
Unknown
Evidence
Unknown

Eruption Statistics & Analysis

MetricValueGlobal RankingSignificance
Total Recorded EruptionsUnknownLowModerately active volcano
Maximum VEIVEI UnknownMinorLocal impact potential
Recent Activity1 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.
fire on brown rocky mountain under gray sky

Einar Jónsson

via Unsplash

an aerial view of a lava flow in the ocean

Anna Muniak

via Unsplash

a body of water with icebergs in it and clouds above

Einar Ingi Sigmundsson

via Unsplash

Other Volcanoes in Iceland

Interesting Facts

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The 2023-2025 Sundhnúkagígar eruptions represent the first volcanic activity on the Reykjanes system in approximately 800 years — the last onshore eruptions were in the 1240s.

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The town of Grindavík (population ~3,800) was evacuated in November 2023 ahead of the eruption series, in one of Iceland's most dramatic modern civil protection operations.

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Lava from the eruptions has entered the outskirts of Grindavík, destroying buildings and raising questions about whether the town can be safely reoccupied.

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The Svartsengi geothermal power plant, which supplies heating and electricity to the entire Reykjanes region, sits within a few kilometers of the active fissures.

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The Blue Lagoon, Iceland's most-visited tourist attraction with over 700,000 annual visitors, has been periodically closed due to its proximity to the eruptions.

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Scientists at IMO believe the current eruption series may continue for years to decades, based on comparison with the 13th-century Reykjanes Fires that lasted approximately 60 years.

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Keflavík International Airport — Iceland's main air gateway — lies only about 20 km north of the active volcanic zone.

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The 1783 submarine eruption produced the ephemeral island of Nyey, which was briefly claimed for Danish sovereignty before wave erosion destroyed it.

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Reykjanes is the only place on Earth where the Mid-Atlantic Ridge — the boundary between the North American and Eurasian tectonic plates — is accessible on land.

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The VEI 4 eruption of 1226-1227 was the largest historically recorded event on the Reykjanes system.

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A persistent magma sill at approximately 4-5 km depth beneath Svartsengi has been feeding repeated dike injections to the surface during the current eruption series.

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Defensive earth and lava barriers have been constructed to protect the Svartsengi power plant and Blue Lagoon — one of the first uses of engineered lava flow diversion in Iceland since the 1973 Heimaey eruption.

Frequently Asked Questions

Is the Reykjanes volcanic system still erupting?
As of 2025, the Reykjanes volcanic system is in an active eruption series. Confirmed eruptions occurred in December 2023 through early 2024, April 2025, and July 2025, all from the Sundhnúkagígar fissure swarm near Svartsengi. Between eruptions, a magma sill at approximately 4-5 km depth reinflates, building toward the next dike injection and fissure eruption. The Icelandic Meteorological Office (IMO) considers this an ongoing volcanic episode that could continue for years to decades, based on the pattern of the 13th-century Reykjanes Fires.
Is Grindavík safe?
Grindavík, a fishing town of approximately 3,800 residents, has been under evacuation advisories during active eruption periods since November 2023. Lava flows from the Sundhnúkagígar fissures have entered the outskirts of the town, destroying several buildings. Ground subsidence and fissuring from dike intrusions have also damaged infrastructure. During quiet periods between eruptions, limited access has been permitted for residents to retrieve belongings, but the long-term viability of the town remains uncertain as scientists expect continued eruptive activity for years to decades.
Will the eruptions affect flights to Iceland?
The Reykjanes eruptions have not caused significant flight disruptions at Keflavík International Airport, which lies approximately 20 km north of the active fissures. The eruptions have been predominantly effusive (lava flows) rather than explosive, producing relatively little ash. This is fundamentally different from the explosive 2010 Eyjafjallajökull eruption that shut down European airspace. However, IMO monitors the situation continuously, and the possibility of more explosive phreatomagmatic activity — if fissures interact with groundwater — cannot be excluded.
Is the Blue Lagoon still open during the eruptions?
The Blue Lagoon has been periodically closed and reopened during the eruption series due to its proximity to the active volcanic fissures and the Svartsengi geothermal field. Access depends on the current eruption status and volcanic gas conditions. Visitors should check the Blue Lagoon's official website and IMO volcanic alerts for the latest access information before planning a visit. Defensive barriers have been constructed to help protect the facility from lava inundation.
How long will the Reykjanes eruptions last?
Scientists at IMO and the University of Iceland believe the current volcanic episode on the Reykjanes Peninsula could continue for years to decades. This assessment is based on comparison with the 13th-century Reykjanes Fires, when the system produced at least eight eruptions over approximately 60 years (1179-1240). The current pattern — repeated inflation of a shallow magma sill followed by fissure eruptions every few months — is consistent with a sustained volcanic episode rather than a single isolated event.
What type of volcano is Reykjanes?
Reykjanes is not a single volcanic cone but rather a fissure volcanic system — a broad area of crater rows, fissures, and small shield volcanoes aligned along the Mid-Atlantic Ridge. This type of volcanism produces basaltic lava flows through linear fissures rather than from a central summit crater. The eruption style is predominantly effusive, with lava fountains and flowing lava rather than explosive ash columns. This makes Reykjanes fundamentally different from Iceland's stratovolcanoes like Hekla or subglacial calderas like Grímsvötn.
Can you see the Reykjanes eruptions?
During active eruption phases, authorized viewing areas have been established at safe distances from the fissures, and tens of thousands of visitors have hiked to vantage points to witness the lava fountains and flows — making these some of the most publicly witnessed eruptions in volcanic history. However, access is strictly controlled by Icelandic authorities and can change rapidly. Visitors should follow all official guidance, as volcanic fissures can open without warning, gas concentrations can be lethal, and ground stability near active lava is unpredictable.
Why is the Reykjanes Peninsula erupting now?
The Reykjanes Peninsula eruptions are driven by the divergence of the North American and Eurasian tectonic plates along the Mid-Atlantic Ridge, which runs directly through the area. The current activity appears to represent the start of a new volcanic cycle after approximately 800 years of quiet. Geological evidence shows that the Reykjanes systems tend to activate in multi-decade episodes — like the Reykjanes Fires of 1179-1240 — separated by centuries of dormancy. A magma sill has been detected at approximately 4-5 km depth beneath Svartsengi, and it periodically feeds dike intrusions that reach the surface as fissure eruptions.