The ongoing fissure eruption in the Geldingadalur valley on the Reykjanes peninsula, Iceland.
After weeks of seismic activity with well over 50,000 earthquakes, a volcanic eruption has started yesterday evening on the Reykjanes peninsula. The eruption started north-east of the town of Grindavík, in a valley called Geldingadalur near Fagradalsfjall mountain, about 30 kilometers (19 miles) south from Reykjavík, the capital and largest city of Iceland. Iceland’s Minister of Justice Aslaug Arna Sigurbjornsdottir shared an image of the night sky glowing bright red, illuminated by the lava.
First images taken during the night and early morning hours by the crew of a Coast Guard helicopter show a 2,6 km long slow-flowing lava flow, feed by a 200 to 500 meters (roughly 1,640 feet) long fissure eruption.
The inland of Reykjanes peninsula is sparsely populated, there are no major towns or villages in imminent danger. The highway between Reykjavík-Keflavík international airport and the capital area, on the northern shore, has been closed by police for the time being. Airspace in a 5-kilometer radius around the ongoing eruption was closed for unmanned aircraft and drones to avoid conflicts with first responders and scientists monitoring the developing situation, and authorities urged people to avoid the eruption site. However, a webcam covers the ongoing eruption via live-stream.
The Icelandic Police Department said it expected volcanic gas pollution to extend as far as the southern coast of the Ölfus municipality, where at least 2,000 people live, almost 50 kilometers (30 miles) away from Reykjavik. The concentration of volcanic gases, like sulfur-dioxide, in the air is not toxic, but can cause irritations in people with pre-existing conditions.
Local media reported that both inbound and outgoing air traffic had been halted from Keflavik International Airport since this morning, a precautionary step, as volcanic ash can damage plane engines. The Icelandic Meteorological Office issued a “code red” warning. A red warning includes the danger of plumes of volcanic ash in the higher layers of the atmosphere, possibly interfering with flight paths.
Exactly ten years ago, the Eyjafjallajökull volcano on the southern tip of Iceland erupted, notoriously disrupting around 900,000 flights across Europe over a period of several weeks.
Volcanic ash is made up from fragments of rock and glass splitters. When this material is sucked by the compressor into the engines of a modern jet aircraft, it will melt in the 2,000°C hot combustion chamber, but quickly re-solidifies on the turbine blades, clogging and eventually blocking the engine.
Estimated six eruption columns per year rise high enough into the stratosphere (15 to 50 kilometers, or 26,000 to 52,000 feet) to endanger air traffic. In the last thirty years, eighty modern jets were damaged by volcanic ash. Ten airplanes experienced temporarily in-flight loss of engine power, losing height rapidly.
Volcanic ash forms by two processes. Sudden and violent degassing of magma, rich in volatiles like carbon-dioxide, water vapor, and other volcanic gases, fragmenting the magma into tiny droplets, or magma encountering water or ice, resulting in steam explosions with the same effect. Volcanism on Iceland is characterized by basaltic magma with low concentrations of volatile gases. Eruptions are generally effusive, with spectacular lava fountains and flows, but few explosions.
The eruption of Eyjafjallajökull happened under a glacier and caused a lot of ash, whereas the current eruption in the Geldingadalur valley is not under an ice sheet and as such likely won’t spew out much ash. A forecast for ash in the air by the Icelandic Meteorological Office shows the volcanic plume moving eastwards, away from airfields and Reykjavík.
So far, the eruption of Fagradalsfjall – as the new volcano was named – is small and does not cause any concern for potential damage to infrastructure or people. No significant amounts of ash have been released, and according to statements by Icelandairs, air traffic will resume soon.
I’m a freelance geologist working mostly in the Eastern Alps. I graduated in 2007 with a project studying how permafrost, that´s frozen soil, is reacting to the more