Bárðarbunga

The Ice Queen

2014-15 Holuhraun Eruption
85 km² Lava Field Size
2,009m Peak Elevation

About Bárðarbunga

Bárðarbunga is a subglacial stratovolcano beneath the Vatnajökull ice cap, rising to ~2,009 m. It has a caldera about 70 km² in area and is part of Iceland's largest volcanic system at ~200 km long. It produced the largest lava eruption in Iceland in over 230 years with the 2014-2015 Holuhraun event.

🌋 Volcanic System

  • Peak elevation: ~2,009 m (Iceland's second highest)
  • Caldera: ~70 km² in area
  • Volcanic system: ~200 km long (Iceland's largest)
  • Eruption frequency: Every 250-600 years typically

🧊 Under the Ice

  • Buried beneath Vatnajökull glacier
  • Ice thickness: up to 850m at summit
  • Creates subglacial volcanic lakes
  • Eruptions can cause massive floods

Holuhraun Eruption 2014-2015

🔥 Iceland's Largest Eruption in 230 Years

The Holuhraun eruption lasted 6 months (August 2014 - February 2015) and created a lava field larger than Manhattan. It was one of the most closely monitored eruptions in history.

Eruption Stats

  • Duration: 181 days (6 months)
  • Lava field: 85 km² (larger than Manhattan)
  • Lava volume: 1.6 km³
  • Fissure length: 1.5 km initially

Impact

  • Massive SO₂ gas emissions
  • Air quality warnings across Iceland
  • Caldera subsided by 65m
  • 16,000+ earthquakes recorded

Why Holuhraun Was Special

Unlike most Icelandic eruptions, Holuhraun occurred on the surface (not under ice), making it safely accessible for scientific study. It became the most monitored effusive eruption in history, with continuous measurements of lava flow, gas emissions, and ground deformation.

Monitoring & Activity

Bárðarbunga is one of Iceland's most closely monitored volcanic systems due to its potential for large-scale eruptions.

📡 Monitoring Systems

  • Dense seismometer network
  • GPS stations track ice surface movement
  • Satellite radar monitoring (InSAR)
  • Regular glacial flood monitoring

🚨 Current Status

  • Active monitoring ongoing
  • Regular seismic activity
  • Caldera still recovering from 2014-15
  • No imminent eruption signs

Historical Eruptions

  • 2014-2015: Holuhraun fissure eruption - 85 km² lava field, largest since Laki
  • 1910: Eruption at the Þjórsá fissure
  • 1862-1864: Activity at the Þjórsá and Veiðivötn fissures
  • 1797: Eruption at the Veiðivötn fissure
  • 1701-1780: Multiple eruptions during this period
  • 1477: VEI 6 eruption produced ashfall reaching Greenland
  • ~870 CE: Vatnaöldur fissure eruption at time of Iceland's settlement

⚠️ January 2025 Seismic Activity

Earthquake swarms in January 2025 included ~130 earthquakes up to magnitude 5.1, suggesting magma accumulation under the caldera. Scientists monitor the system closely for signs of potential future eruptions.

Visiting Holuhraun Lava Field

The Holuhraun lava field is located in Iceland's remote highlands, north of Vatnajökull glacier.

Access

  • Location: North of Vatnajökull
  • Access: F-road (4WD required)
  • Season: Summer only (July-September)
  • Distance: ~40km from Ring Road

What to Expect

  • Vast black lava field stretching to horizon
  • Steam rising from cooling lava
  • Colorful sulfur deposits
  • Dramatic fissure formations

⚠️ Safety Note

The Holuhraun lava field is in a remote highland area accessible only by 4WD vehicle in summer. Check road conditions at road.is and weather at vedur.is before attempting to visit. Gas emissions may still be present in some areas.