The new eruption, now called the “Geldingadalsgos” eruption by the Icelandic media, continues steadily. It has been producing slowly advancing lava flows inside the Geldingadal valley. The Icelandic Met Office and local news outlets published many new photos from the ongoing eruption this morning.
The isolated location in Geldingadalur valley means there is no immediate danger to any infrastructure. Volcanic gases are not currently being blown over any towns or villages and are unlikely to cause any problems even if the wind changes direction, according to the Icelandic Met Office (IMO).
Six or more vents above the eruptive fissure have formed smaller and one larger spatter cones, where the activity is concentrated now, mainly from the largest one in the middle, which likely will become the main (and only) active vent in a short time.
There is little lava fountaining from the vents, only mild spattering, but largely degassed magma erupts steadily into flows directed into two main flow fields, a narrower one to the southwest and a broader field to the north and northwest.
Both lava fields have reached approx. 500 m length and the total area covered by new lava was estimated to be around 0.1 km2 with an average thickness of about 10 m, thus giving a total volume of 1 million cubic m and an average eruption rate of approx. 15 m3 per second, similar to the estimates done previously of the magma influx into the dike that is now feeding the eruption.
How long might the eruption continue?
Nobody can know for sure how long this eruption can continue, but most scientists are currently thinking that it might be several weeks or months. It largely depends on how much magma is available (and able to reach the surface), and how long the magma resupply into the dike continues, and how long the current magma pathways are stable (and not changed by new earthquakes, opening of fractures etc).
If the reported dike was 10 km long, about 5 km tall and 1 m wide, it would contain approx. 50 million cubic meters, enough to let the eruption continue for several weeks at the current effusion rate, if about half of what is stored in it now would erupt, not counting the volume added by ongoing supply from deeper levels.
What about the earthquakes?
Earthquakes continue at reduced rate – as lava is flowing freely now, it doesn’t need to break rocks to generate new paths. In fact, no significant shallow quakes have been detected in the area since the eruption. However, deeper earthquakes at 4-6 km depth continue,- something that suggests that in the lower parts of the dike, things are not stable yet and the eruption might evolve in different ways than continue just as it is now.
Ancient burial site threatened by lava flows
As the valley where the eruption is taking place is home to an ancient burial site dating back to before the year 1000, a spot where the remains of the Norse settler Ísólfur frá Ísólfsstöðum lie, now threatened to be covered forever, archeologists rushed into place yesterday to do some “rescue excavations”.