Magma volume under Svartsengi is reaching a level similar to before the last eruptions
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Updated 23. February at 15:00 UTC
Model calculations indicate that approximately 5 million cubic meters of magma had recharged to the Svartsengi reservoir as of 22 February. Considering the trend observed before previous volcanic eruptions in the Sundhnúkur crater row, the likelihood of an eruption is very high once the volume reaches between 8-13 million cubic meters (derived from joint InSAR-GNSS models). Based on the results of the model calculations, this could occur early next week if magma accumulation continues at the current rate.
It should be noted that there is a degree of uncertainty in this interpretation, and it cannot be assumed that the behavior will be identical to the past eruptions here. Also, as the magma plumbing system evolves, we cannot rule out the possibility that the volume of magma required to trigger a new diking event and/or eruption may become reduced.
Additionally, there is a possibility that magma could migrate from a dike intrusion occurs within this region without resulting in a volcanic eruption.
If an eruption occurs, scientists estimate that magma will most likely propagate from the reservoir beneath Svartsengi towards Sundhnúkur crater row, resulting in lava fountaining and lava flows in the area between Stóra-Skógfell and Hagafell. The primary signal of ascending magma is a sudden increase in seismic activity with many localized, small magnitude earthquakes. Considering the previous volcanic eruptions in the area, an eruption could start with very little warning (less than 30 minutes), depending on where magma reaches the surface on the Sundhnúkur crater row.
Likely scenarios
Eruption between Sýlingarfell and Stóra-Skógfell - As occurred on Dec. 18, 2023, and Feb. 8, 2024.
Eruption by Hagafell – As occurred on Jan. 14, 2024.
Eruption inside of the lava barriers around Grindavík
Although there is a clear indication of uplift in the Svartsengi-Þórbjörn area (related to magma recharge of this reservoir) this does not mean that it is the most likely location for an eruption to start. This is because the magma reservoir is currently failing on its northeastern edge feeding dike propagations which are initiated between Stóra-Skógfell- and Sundhnúkur crater row. In a scenario where magma ascends towards the surface directly from the Svartsengi reservoir, it is estimated that the first signs of magma migration would be detected 4-7 hours before magma reaches the surface.
Please note that these scenarios are based on interpretations of the latest data and the observed development of the previous events at the Sundhnúkur crater row area. Uncertainty must be accounted for in this interpretation, as it is only based on a few events.
Updated 23. February at 9:30 UTC
Seismic activity in the unrest area north of Grindavík remains minimal. About 20 small earthquakes have been detected on a 24-hour basis for the past days.
Magma accumulation beneath Svartsengi continues and the pace of the accumulation has been quite steady. This is a similar trend as has been observed before the previous volcanic eruptions.
The event which started at the end of October 2023 with an inflation at Svartsengi thus continues. Whilst magma accumulation persists, another volcanic eruption is expected in similar areas as before.
Should magma accumulation continue at the current pace, the amount will reach a threshold believed necessary to trigger a dyke propagation and even an eruption, by next week. The amount of magma accumulated beneath Svartsengi before previous eruptions is estimated to have been 8-13 million m3. New model calculations are underway to obtain a better understanding of how much magma has now been accumulated.
At the moment, it is not considered necessary to raise the hazard level in the area and thus the hazard assessment issued by IMO remains unchanged.
The hazard assessment will be updated on Monday 26 Feb. and should the development continue at a similar rate as now, hazard levels in zones will be raised as more magma will accumulate and thus there is a higher likelihood of an eruption.