Bárðarbunga

Background

History & Background

Bárðarbunga's history is deeply intertwined with the formation of Iceland itself, a land perpetually shaped by its position on the Mid-Atlantic Ridge where the North American and Eurasian tectonic plates diverge. This massive stratovolcano, reaching an elevation of 2009 meters, has been active for at least the past 10,000 years, with numerous eruptions both subglacial and effusive. Its caldera, approximately 70 square kilometers in area, lies beneath hundreds of meters of ice, making its eruptions particularly complex and often leading to significant meltwater floods. One of its most notable recent events was the 2014-2015 eruption, which began with intense seismic activity and resulted in a sustained effusive eruption in the Holuhraun lava field, just north of the Vatnajökull glacier. This eruption produced a vast new lava field, covering over 85 square kilometers, and released significant amounts of sulfur dioxide, impacting air quality across parts of Europe. This event provided scientists with an unprecedented opportunity to study a large-scale basaltic eruption in real-time, offering invaluable insights into volcanic processes and their environmental effects.

Bárðarbunga is a major subglacial volcanic system beneath the Vatnajökull ice cap. Its activity is monitored closely because eruptions can interact with glacial ice and generate meltwater floods. The central caldera is not a normal visitor destination; travellers experience the wider volcanic and glacial landscape from permitted highland routes and areas around Vatnajökull.