🌋VolcanoAtlas

Jan Mayen (Beerenberg)

The World's Northernmost Active Volcano

Elevation

2,277 m

Last Eruption

1985

Type

Stratovolcano

Country

Norway

Location

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Volcanic Hazards & Risk Assessment

Primary Hazards

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

Risk Level

Population at RiskLow
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 Activity41 years agoRecentRecently active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Watch
Dormant but monitored. Capable of renewed activity.

Interesting Facts

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Beerenberg is the northernmost active subaerial volcano on Earth, located at 71°N latitude — well within the Arctic Circle and farther north than any point on the Alaskan or Siberian mainland.

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The 1970 eruption went undetected for three days by nearly 40 people stationed just 30 km away, finally noticed only when commercial aircraft pilots reported the eruption cloud.

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More than 20 glaciers cover approximately 30% of Jan Mayen's surface, and some extend their tongues to sea level — making Beerenberg one of the rare places where active lava flows can interact directly with glacial ice.

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The 1985 eruption lasted only 35–40 hours but produced approximately 7 million m³ of lava — enough to bury a football pitch under 1,400 m of rock.

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Jan Mayen's sole human population consists of approximately 18 Norwegian military and meteorological personnel who rotate through the station at Olonkinbyen.

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Beerenberg's name means 'Bear Mountain' in Dutch, given by 17th-century whalers who encountered polar bears on the island's shores.

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The island sits at the junction of three major tectonic features: the Mohn's Ridge, the Jan Mayen Fracture Zone, and the Jan Mayen Ridge microcontinent — a fragment of Greenland separated 55 million years ago.

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During the 1985 eruption, observers in a Norwegian Coast Guard helicopter reported the Arctic sea 'boiling' up to 150 m from shore where lava entered the ocean.

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James Wordie, who had served on Shackleton's ill-fated Endurance expedition to Antarctica, was among the first people to reach Beerenberg's summit in 1921.

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Between 600 and 800 earthquakes per day were recorded during the 1970 eruption, with the volcanic fissure stretching 6 km across the northeastern flank.

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Jan Mayen is approximately 53 km long but only a few hundred meters wide at the narrow isthmus separating the Beerenberg volcano from the Sør-Jan volcanic field.

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The Sør-Jan volcanic complex produces trachytic lavas — a more evolved, silica-rich magma chemistry distinct from Beerenberg's basaltic output — indicating two separate magmatic plumbing systems beneath the island.

Frequently Asked Questions

Is Jan Mayen's Beerenberg volcano still active?
Yes, Beerenberg is classified as an active volcano. Its most recent eruption occurred on January 6–9, 1985, making it Norway's only historically active volcano. Slight but continuous steam emission has been observed from the summit region since the 1970 eruption cycle. The Norwegian Polar Institute states that there is a constant threat of new eruptions and earthquakes. With an estimated eruption frequency of 150 ± 75 years for major events — and three eruptions clustered between 1970 and 1985 — Beerenberg should be considered capable of erupting again with potentially limited warning.
When did Jan Mayen last erupt?
The most recent eruption of Beerenberg volcano on Jan Mayen began on January 6, 1985, and lasted approximately 35–40 hours. The eruption was preceded by earthquakes up to magnitude 5.4, and lava erupted from a 1-km-long fissure on the extreme northeastern corner of the island. Approximately 7 million cubic meters of basaltic lava flowed north into the Arctic sea. Before 1985, eruptions occurred in 1973 (VEI 1) and 1970–1971 (VEI 3), representing a cluster of activity after 120 years of quiescence.
How tall is Beerenberg?
Beerenberg stands 2,277 m (7,470 ft) above sea level, making it the highest point on Jan Mayen and the tallest mountain in the Arctic (excluding Greenland's ice-covered peaks and non-volcanic mountains). The Smithsonian Global Volcanism Program records the summit elevation as 2,197 m, though Norwegian sources consistently cite 2,277 m. The discrepancy may reflect different measurement points or the effects of glacial ice on the summit. The mountain's base extends roughly 25 km in diameter at sea level, with the summit cone rising steeply above a broader shield volcano base.
What type of volcano is Beerenberg?
Beerenberg is a basaltic stratovolcano (composite volcano) built upon an older shield volcano base. The structural distinction is visible in the mountain's profile: gentle ~15° slopes on the lower flanks (the shield phase) give way to steeper ~30° slopes on the upper cone (the stratocone phase). The volcano is composed primarily of basaltic lava flows with minor tephra layers and is dotted with numerous parasitic cinder cones along flank fissures. The southwestern part of Jan Mayen (Sør-Jan) hosts a separate volcanic field of cinder cones and trachytic lava domes.
Can you visit Jan Mayen?
Visiting Jan Mayen is possible but extremely difficult. The island is a Norwegian dependency with restricted access, and there is no civilian airport or harbor for large ships. Access typically requires either Norwegian military authorization or passage on expedition cruise ships that occasionally include Jan Mayen in Arctic itineraries — though weather frequently prevents landings. Shore visits, when possible, are conducted by Zodiac in the Sør-Jan area. Climbing Beerenberg is an extreme mountaineering challenge requiring full glacier equipment and favorable weather that may not appear for days. Fewer than a handful of expeditions attempt the summit each year.
Why is Jan Mayen volcanic?
Jan Mayen's volcanism results from its position at the junction of three major tectonic features: the Mohn's Ridge (the northward continuation of the Mid-Atlantic Ridge, where the North American and Eurasian plates diverge), the Jan Mayen Fracture Zone (a transform fault), and the Jan Mayen Ridge microcontinent (a fragment of Greenland that rifted away approximately 55 million years ago). This tectonic triple junction creates complex stress patterns and enhanced mantle upwelling that drive magma generation. Unlike Iceland, which benefits from an additional deep mantle hotspot, Jan Mayen's volcanism is primarily driven by ridge-transform dynamics.
How many people live on Jan Mayen?
Approximately 18 people live on Jan Mayen at any given time, all Norwegian military and meteorological personnel who rotate through the station at Olonkinbyen on the southwestern coast. There is no permanent civilian population and never has been. The station's primary functions are weather observation (critical for North Atlantic aviation and shipping forecasts), seismic monitoring, and operation of navigation infrastructure. The settlement lies approximately 30 km from Beerenberg's summit, within potential range of tephra fall and seismic effects from a large eruption.
What would happen if Beerenberg had a large eruption today?
A large eruption of Beerenberg would primarily threaten the 18 station personnel on the island through tephra fall, seismic activity, and potentially jökulhlaups (glacial outburst floods) if the eruption occurred beneath the extensive glacier cover. Ash clouds could disrupt North Atlantic aviation corridors between Europe and North America. Lava flows from flank fissures could reach the sea rapidly, as in 1970 and 1985. An evacuation would depend on weather conditions and the availability of Norwegian military or Coast Guard transport — which in Arctic winter conditions could be severely delayed. The 2022 Frontiers in Earth Science hazard assessment produced the first comprehensive volcanic hazard maps for the island.