Today (28-May-2022) at 08:06 UTC an earthquake with magnitude of Mw4,4 or Mw4,7 (EMSC information can be found here) took place in Bárðarbunga volcano.
Earthquake activity in Bárðarbunga volcano. Copyright of this image belongs to Icelandic Met Office.
This earthquake activity is because of inflation in Bárðarbunga volcano magma chamber. That was emptied after the eruption in 2014 – 2015 and that resulted in collapse of Bárðarbunga volcano by drop of some 60 meters. This inflation now is reversing that process slowly. It is going to be decades until Bárðarbunga volcano erupts again because of this collapse.
On Thursday 26-May-2022 at 20:11 UTC an earthquake with magnitude of Mw3,5. I think this earthquake was maybe felt in populated areas closest to the earthquake. This earthquake was out in the ocean, a good distance from land.
Earthquake activity on Reykjanes ridge and Reykjanes peninsula. Copyright of this image belongs to Icelandic Met Office.
This earthquake possibly is part of the earthquake activity that is happening in Reykjanes peninsula and Reykjanes ridge. It is more difficult to know what is going on in the ocean, than on land.
Posts are going to get delayed for the next few days because I am moving to Denmark.
Today (23-May-2022) at 07:14 UTC an earthquake with magnitude of Mw3,5 took place north-east of Grindavík town. This earthquake was felt in Grindavík and in Reykjavík. The earthquake was located in a area that is either inflating or on the edge of area that is inflating.
Earthquake activity on the Reykjanes peninsula close to Grindavík. Copyright of this image belongs to Icelandic Met Office.
According to Icelandic Met Office news, the inflation around Þorbjörn mountain since the start of this earthquake activity is currently at 45mm. I don’t know how much inflation the crust can take in this area before an eruption starts in this area. Any eruption in this area is probably going to start with few craters that shut down with time and then there is just one crater that erupts until the eruption ends.
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Today (22-May-2022) at 09:53 and 09:57 UTC earthquakes with magnitude of Mw3,5 and Mw3,6 took place north-west of Grindavík town. This earthquake was felt and did wake up people according to the news.
Earthquake activity close to Grindavík town. Copyright of this image belongs to Icelandic Met Office.
There is no signs that this earthquake activity is slowing down. It does come in waves according to Icelandic Met Office. This means that there are period of high activity with low activity between. Currently, at the writing of this article, there is a low activity period ongoing.
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Today (20-May-2022) around 18:00 UTC the earthquake activity off the coast of Reykjanestá, that is part of Reykjanes volcano, increased again after few days of little earthquake activity. The earthquake swarm is ongoing and always changing so this article is going to be short because of that.
Earthquake swarm on the Reykjanes ridge, close to Reykjanestá. Copyright of this image belongs to Icelandic Met Office.
Largest earthquake so far had a magnitude of Mw3,8 and the second largest earthquake had a magnitude of Mw3,5. The Mw3,8 earthquake was felt in Grindavík and on nearby towns on Reykjanes peninsula. A Mw3,0 earthquake took place just north of Grindavík and was felt in the town.
Yesterday (18-May-2022) I forgot to write about the earthquake activity that is ongoing north of Grindavík town. This earthquake activity is either in the new dyke that has formed or ongoing path of the dyke in Svartsengi that has now reached north of Grindavík town. I don’t know what applies here. Skjálftalísa map that Icelandic Met Office has strongly suggests a second dyke, but the results are bit unclear. In the area east of Þorbjörn is a older eruption fissure, I don’t know when it erupted, but it might have been as early as 12th to 13th century.
Six green stars north of Grindavík town. Copyright of this image belongs to Icelandic Met Office.
Yesterday (18-May-2022) total of five earthquakes happened with magnitude larger than Mw3,0. Largest earthquake had a magnitude of Mw3,5. Today (19-May-2022) at the writing of this article, only one earthquake with magnitude of Mw3,0 has happened. Earthquake activity seems to be slowing down. I am not sure why that is.
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According to news today (18-May-2022) and based on recent measurements, a magma dyke has formed between Þorbjörn mountain and Eldvörp on Reykjanes peninsula. Eldvörp on Reykjanes peninsula where formed during last eruption cycle in the volcano of Reykjanes during 12th and early 13th century, exact times are poorly known. This is in a volcano named Reykjanes and is not connected to Krýsuvík-Trölladyngja volcano that erupted in 2021 (Fagradalsfjall mountain).
The dyke is shallow and narrow according the news that quote scientists from University of Iceland, Earth science department and Icelandic Met Office. The length of dyke is 7 to 9 km and depth is down to 4 to 8 km (?). This also shows up in the GPS data and other data that Icelandic Met Office has access to (I don’t have this level of access).
Earthquake activity north of Grindavík town. Copyright of this image belongs to Icelandic Met Office.
It is not possible to know when a eruption start or in what area. The main risk areas now are Blue Lagoon, HS hydrothermal energy thermal plant. The town of Grindavík is slightly south of this and is possibly in danger. How this goes depends on where the eruption starts and how large it is going to be. Smaller eruption is less of a problem than a big eruption in this area. All that can be done now is to continue to monitor the situation.
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This is a short article about ongoing activity in Reykjanes volcano.
At 17:38 UTC an magnitude Mw4,3 earthquake took place in Eldvörp crater row. This earthquake was felt over a wide area of south Iceland and on Reykjanes peninsula.
Strong earthquake activity west of Grindavík town. Copyright of this image belongs to Icelandic Met Office.
As it currently is, the earthquake activity in this area is going to continue to increase until an eruption starts. When that might happen is not something I can predict.
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Updated at 20:52. Icelandic Met Office downgraded this earthquake when it was reviewed again. This article has been updated in accordance with the new information.
Today (15-May-2022) a strong earthquake activity started in Eldvörp crater crow west of Grindavík town. Largest earthquake at the writing of this article had a magnitude of Mw4,1. Stronger earthquakes are a possibility. Total of five earthquakes with magnitude stronger than Mw3,0 have taken place since 11:00 UTC this morning. More than 100 earthquakes that are smaller in magnitude have happened since then.
Earthquakes in Reykjanes volcano in Eldvörp crater row. Copyright of this image belongs to Icelandic Met Office.
I am not seeing any clear signs that this earthquake activity is because of tectonic activity. This earthquake activity is in my personal view because of magma trying to find a path to the surface, something that it seems to struggle with. A process that was also seen just before the eruption in Fagradalsfjall mountain. The difference now is that an eruption in this area might be a magnitude or two larger than an eruption in Fagradalsfjall mountain, until an eruption starts, this is just a speculation. It is impossible to know when an eruption is going to start at this location, or if it is going to start. That is the most likely outcome of all this, but volcanoes remain unpredictable.
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There is a an ongoing earthquake swarm in Reykjanes volcano and it has been going on for more than a week now. Location of this swarm has moved a little and the main earthquake activity is now at Reykjanestá area out in the ocean. There have been five earthquakes with magnitude above Mw3,0 today (13-May-2022) and the largest so far had a magnitude of Mw3,5.
Earthquake activity on Reykjanes ridge and on Reykjanes peninsula. Copyright of this image belongs to Icelandic Met Office.
This earthquake activity suggests two things. Either the magma has not been able to find a path to the surface close to Grindavík town. The second option is that there are two dyke intrusions happening in Reykjanes volcano. This earthquake activity slows down but never fully stops it seems. It is unclear why that happens. I am expecting earthquake activity to get stronger until an eruption starts somewhere in Reykjanes volcano.
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