When the Bárðarbunga volcano beneath Iceland's Vatnajökull ice cap reawakened in August 2014, scientists got an opportunity to monitor how the magma flowed through cracks in the rock away from the volcano.
Although it has a long history of eruptions, Bárðarbunga has been increasingly restless since 2005, including a dynamic period in August and September of this year, when more than 22,000 earthquakes were recorded in or around the volcano in just four weeks, due to stress being released as magma forced its way through the rock.
The molten rock formed vertical sheet-like features known as dykes, which force the surrounding rock apart. Using GPS and satellite measurements, the team were able to track the path of the magma for over 45 kilometers before it reached a point where it began to erupt, and continues to do so to this day. The rate of dyke propagation was variable and slowed as the magma reached natural barriers, which were overcome by the build-up of pressure, creating a new segment.
Bárðarbunga volcano October 2014. Source: youtube.com @gisligisla1973
The dyke grows in segments, breaking through from one to the next by the build up of pressure. This explains how focused upwelling of magma under central volcanoes is effectively redistributed over large distances to create new upper crust at divergent plate boundaries, the authors conclude.
Study co-author Professor Andy Hooper from the Centre for Observation and Modelling of Earthquakes, volcanoes and Tectonics (COMET) at the University of Leeds explained,"New crust forms where two tectonic plates are moving away from each other. Mostly this happens beneath the oceans, where it is difficult to observe. However, in Iceland this happens beneath dry land. The events leading to the eruption in August 2014 are the first time that such a rifting episode has occurred there and been observed with modern tools, like GPS and satellite radar."
As well as the dyke, the team found 'ice cauldrons' - shallow depressions in the ice with circular crevasses, where the base of the glacier had been melted by magma. In addition, radar measurements showed that the ice inside Bárðarbunga's crater had sunk by 16 meters, as the volcano floor collapsed.
PhD student Karsten Spaans from the University of Leeds, a co-author of the study, added, "Using radar measurements from space, we can form an image of caldera movement occurring in one day. Usually we expect to see just noise in the image, but we were amazed to see up to 55cm of subsidence."
Like other liquids, magma flows along the path of least resistance, which explains why the dyke at Bárðarbunga changed direction as it progressed. Magma flow was influenced mostly by the lie of the land to start with, but as it moved away from the steeper slopes, the influence of plate movements became more important.
Summarizing the findings, Hooper said, "Our observations of this event showed that the magma injected into the crust took an incredibly roundabout path and proceeded in fits and starts.
"Initially we were surprised at this complexity, but it turns out we can explain all the twists and turns with a relatively simple model, which considers just the pressure of rock and ice above, and the pull exerted by the plates moving apart."
Source: University of Leeds