Yesterday (11-August-2021) there was a earthquake swarm on Reykjanes ridge. This earthquake swarm was not felt because of distance from the coastline.
Largest earthquake in this swarm had a magnitude of mb4,4 according to EMSC. Information about this earthquake can be found here. The distance from the SIL network made it difficult to know when this earthquake swarm started and stopped.
It is unclear if this part of the activity period that Reykjanes peninsula and Reykjanes ridge is now entering and is going to last for few centuries.
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During the night and today on 5-Augustu-2021 an earthquake swarm took place in the Reykjanes volcano.
Largest earthquake in this swarm had a magnitude of Mw3,0 and other earthquakes at the writing of this article have been smaller. That can change without warning. Currently there is a possibly that this earthquake swarm is over.
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At midnight on 1-August-2021 an earthquake swarm seems to have started deep on the Reykjanes ridge. The current distance seems to be around 220 km away from Reykjavík or 190 km from Grindavík town. At this distance the location from Icelandic Met Office are not accurate. At the writing of this article the earthquake swarm seems to be ongoing.
Largest earthquake recorded at the writing of this article had a magnitude of Mw5,2 and the rest of the earthquakes have magnitude between Mw4,0 and Mw4,8. Overview of this earthquake activity can be found here on EMSC website. This links works as I publish this article. How long it is going to work I don’t know.
The current distance makes it impossible to know for sure what is going on at this location. The pattern of this earthquake activity suggests that this might be earthquake activity because of magma movement in the crust, but there is not any way to confirm this because of the location. Even if there is an eruption at this location it won’t make any difference to the surface of the ocean, since depth of the ocean at this location is more than 1 km. I don’t know the exact depth.
This is a short update on the eruption in Fagradalsfjall mountain in Krýsuvík-Trölladyngja volcano system.
There has not been any major change since last update. In this week four new craters started erupting and I write an article about that earlier in this week for more details.
It was reported today (16-April-2021) that lava has now started to flow outside of Geldingadalir and to the east. This lava is now flowing over a walking path that people used to get close to the eruption. Getting close to the eruption might not be possible any more. There is also a chance that lava is going to is going to flow to the south of the craters more than it already has done.
Swarm of small earthquakes took place north-east in Fagradalsfjall mountain early morning around 06:00 UTC. Largest of those earthquakes had a magnitude of Mw2,8.
There is no sign of the eruption ending.
There continues to be a high risk of new vents opening up and start erupting without warning.
There are no more reports this week outside of what I did write about what was happening earlier in the week. If anything major happens I am going to post an update soon as possible.
Today (29-December-2020) an earthquake swarm took place in Reykjanes volcano. This was just small earthquakes but the amount is considerable. This earthquake activity happens because of magma inflation in this area.
Earthquake activity in Reykjanes volcano. Copyright of this image belongs to Icelandic Met Office.
Today (29-December-2020) and earthquake with magnitude of Mw3,1 took place on Reykjanes ridge. This earthquake was far out in the ocean. Only one other smaller earthquake seems to have happened in that same area after the largest earthquake. Otherwise there has not been any more earthquake activity today out on the Reykjanes ridge.
Earthquake activity on Reykjanes ridge. Copyright of this image belongs to Icelandic Met Office.
It was reported by Icelandic Met Office at 22:20 UTC that people had been noticing more gas smell close to a small lake called Grænavatn. This suggest that magma might be on the move in the crust. It is currently difficult to be sure at writing of this article. This would be inside the volcano of Reykjanes.
Grænavatn lake. Copyright of this image belongs to Google Earth / Google.
Earthquake activity on the Reykjanes peninsula at midnight 21-October-2020. Copyright of this image belongs to Icelandic Met Office.
At the writing of this article there has not been any change in harmonic tremor on nearby SIL stations. If magma is about to move that is possibly going to happen without much warning but this difficult to know for sure at the writing of this article.
Since around 06:00 this morning (13-June-2020) a sharp increase in earthquake activity took place north of Grindavík town. The most dense earthquake swarm was located west of the Blue lagoon with other minor swarms in other nearby areas. The active volcano is Reykjanes and Svartsengi (no Global Volcanism profile). Map can be found here and here (go to Höggunarkort).
The clusters of earthquake activity close to Grindavík town. This map can be found here (Icelandic only). Copyright of this image belongs to Icelandic Met Office.
Current earthquake activity close to Grindavík town. Copyright of this image belongs to Icelandic Met Office.
Largest earthquakes at the writing of this article have a magnitude of Mw3,5 (at 20:27 UTC) but since this earthquake swarm in ongoing that number can change without warning.
There was also considerable noise during the earthquake swarm earlier. Suggesting that something is going on but I do not know what might be for now. The noise results in the blue band thickens during the earthquake swarm.
The termor plot during the earthquake swarm. Copyright of this image belongs to Icelandic Met Office.
Current GPS data (can be viewed here) doesn’t show any major changes at the writing of this article. That might change in next few days.
This is the first article on the Iceland geology new domain and new hosting location. I’ve resolved most problems but few remains that I am working on resolving. Please report any problems in a comment here or send me an email to volcano [at] icelandgeology [dot] net. I have updated the email postlist for those who use it. Please check your spam folders and update your rules for the new addresses that are now being used.
Over the weekend there has been a earthquake swarm in the Reykjanes volcano. Largest earthquake in this swarm had a magnitude of Mw2,6 on Saturday 06-June-2020 at 01:01 UTC. Other earthquakes have been smaller in magnitude. Around 220 earthquakes have been recorded at the writing of this article.
The earthquake activity in the volcano called Reykjanes and Svartsengi (Þorbjörn). Copyright of this image belongs to Icelandic Met Office.
The reason for this earthquake swarm is inflation that has been increasing in recent days according to GPS data that is not yet corrected or verified. That GPS data can be found here. This inflation increases the risk of larger earthquake in next few days.
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Since early this morning (18-May-2020) earthquake activity has been increasing in Reykjanes volcano. For the last several weeks there has been a deflation taking place in the volcanoes from Krýsuvík (possibly) and to Reykjanes volcano. Such event is to be expected with a rift volcanoes (see Krafla volcano 1980 – 1984 eruptions).
Current earthquake activity in the Reykjanes volcano and Þorbjörn mountain. Copyright of this image belongs to Icelandic Met Office.
Other than this minor activity it has been quiet in Iceland for the last month. This happens regularly in Iceland. This quiet time might last a while longer.
Please remember to support my work with donations. Support is still needed when things are quiet in Iceland. Please see the pinned article for more details. Thanks for the support. 🙂
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