Day: January 7, 2017

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Earthquakes in Bárðarbunga volcano

On the 4th and 6th of January 2017 earthquakes took place in Bárðarbunga volcano. The earthquake on 4th of January had the magnitude of 3,3 (I think) and the earthquake on the 6th of January had the magnitude of 3,5. Both earthquakes where inside the crater of Bárðarbunga volcano, along the fault rims. The reason for this earthquake activity is the inflation of Bárðarbunga volcano, that appears to be rather rapid and mostly steady process. Influx of magma happens in pulses and those pulses are in different size and how long they last.


The earthquake activity in Bárðarbunga volcano. Copyright of this image belongs to Icelandic Met Office.

This type of earthquake activity is a regular feature of Bárðarbunga volcano at the moment. I don’t expect that to change any time soon. What might change is the magnitude of the earthquakes happening, I suspect that with time they are going to get more rare but larger in magnitude instead.

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Earthquakes in Katla volcano

On the 5th of January 2017 a magnitude 3,5 earthquake took place in Katla volcano. This earthquake happening in January is extremely rare thing, since Katla volcano is normally quiet this time of the year. That seems to be over for now.


Earthquake activity in Katla volcano. Copyright of this image belongs to Icelandic Met Office.

This earthquake was the strong earthquake in a minor swarm that took place in Katla volcano during that day. Since then the activity has been mostly quiet. Bad weather is however interfering with detection of the earthquakes in most of Iceland, a storm is happening 1 to 2 days at the moment.

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The earthquake swarm in Hengill volcano

On the 4th of January 2017 a earthquake swarm took place in Hengill volcano. Largest earthquake had the magnitude of 3,7 and the second earthquake had the magnitude of 2,8. The largest earthquakes where felt in Reykjavík, Hveragerði and Selfoss towns (mostly). In total of 150 earthquakes took place in this earthquake swarm.


The earthquake swarm in Hengill volcano from 4th of January 2017. Copyright of this image belongs to Icelandic Met Office.

This earthquake swarm was due to a process called rifting, this means that where the earthquake swarm is happening the ground is dropping and cracking at the same time. This over time forms a rift valley (like Þingvellir). The area from Hveravellir and south into the ocean of the Reykjanes ridge is all just one big rift valley. Far as I know a period of high earthquake activity can happen in this area, last time this happened sometimes around the middle of 19th century with possible activity sometimes in the 20th (early) century. Since then it has been mostly quiet.

In the year 1789 (source in Icelandic, 1973) the area around Þingvallavatn lake dropped around 63 cm (that estimate is not accurate and it is estimated that it was far more) in a earthquake swarm. When this is going to happen next time is impossible to know.

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