This is a short update on the eruption in Fagradalsfjall mountain in Krýsuvík-Trölladyngja volcano system.
Last 24 hours have been busy in the eruption. Here are highlights of what has happened best to my knowledge.
New fissure opened up and started erupting between the Geldingadalir eruption, second day of Easter eruption and the new eruption fissure is between the two.
The lava fields have now merged and are now one large lava field from Geldingadalir down to Meradalir valleys.
The eruption continues at the same slow rate as before even with several new vents erupting.
Morgunblaðið lost their first web camera to the lava flow (news can be found here in Icelandic). Icelandic Met Office had hardware close to the new lava flow. I don’t know if that hardware was saved from the lava flow but it was planned attempt to do so before it was lost to the lava.
The fissures might merge at future point and start erupting at one large fissure eruption. It is impossible to know if that is going to happen or when that might happen.
There has not been any deflation detected in the GPS data after the eruption started. That GPS data can be viewed here.
New fissures have been detected north of the crater that started erupting on 5-April-2021. Those fissure might start erupting without warning.
There is a risk of the eruption also going south-west and opening up fissures there. That has not yet happened but the possibility remains as a high risk possibility.
The situation is difficult to predict and new fissures can open up without warning. If nothing major happens then next update is going to be Friday 9-April-2021 on the eruption.
This is a short update and second update for 6-April-2021 for Fagradalsfjall mountain that is part of Krýsuvík-Trölladyngju volcano system.
During the night a new fissure was discovered between the new eruption and the old eruption. The fissure is about 150 meters long and there is hot air coming up from it.
There are reports of a new fissure north of the new eruption and land has been sinking down at that location. No other changes have been reported at the writing of this article.
The lava going down into Meradalir valley slows down once it is there because it cools down quickly once it is there. There is a lava river going down in the Meradalir valley and that lava is moving quickly.
It is now estimated that this is a start of a long volcano activity period on Reykjanes peninsula that is going to last for centuries with breaks of 10 to 20 years between active periods of 30 to 50 years.
The situation is currently changes often during the day and the night and the risk of a new eruptions starting without any warning is now extremely high.
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Yesterday (5-April-2021) from 17:12 UTC until 17:36 UTC. This where all smaller earthquakes and according to Icelandic Met Office (Kristín on twitter) this area last had this earthquake swarm in this area eight years ago just south-east of Katla volcano.
The earthquake activity south-east of Katla volcano. Copyright of this image belongs to Icelandic Met Office.
This earthquake activity at this location has never resulted in an volcanic eruption in this location during historical times. The depth of this earthquakes was mostly around 19 km and magnitude was from Mw0,7 to Mw1,0.
On Sunday (4-April-2021) a small of small earthquakes took place in Öræfajökull volcano. Most of the earthquakes that happened where deep, with most depth at 11,3 km.
Earthquake activity in Öræfajökull volcano. Copyright of this image belongs to Icelandic Met Office.
It is unclear if this means anything at this point. Earthquake activity in Öræfajökull volcano at this point has been slow to start and happens without much warning as is. This might be an early sign that more activity is ahead in Öræfajökull volcano but only time is going to make it clear if that is the case.
This is a short update on the eruption in Fagradalsfjall mountain as it is part of Krýsuvík-Trölladyngja volcano.
There has been a slight increase in micro-earthquake activity along the dyke after the new fissures opened up in Fagradalsfjall mountain. Most of them are interestingly forced on a area close to Keilir mountain.
The earthquake activity on the Reykjanes peninsula. Copyright of this image belongs to Icelandic Met Office.
It has been reported that lava flow from the new and old eruption site is now more than what was most at the old eruption site (Geldingadalir valley). It is now estimated to be total 10m3/second.
Craters are building up at the new eruption site. That might change the lava flow long term and there is a risk that it is going to flow towards Geldingadalir valley when that change in lava flow happens.
There is a high risk of new fissures opening up both north and south of Geldingadalir valley (1st eruption) and north of Fagradalsfjall mountain eruption (2nd eruption).
Lava is now flowing into Meradalir valley. That valley is far larger then Geldingadalir valley and won’t be filled up easily. There seems to be more water in this valley and that might result in lava explosions if the lava gets that far down into the valley.
Currently there are no other new information that I can find. Next update should be on Friday 9th April 2021 unless something major happens.
New fissure started to open up at around 11:37 UTC on 5-April-2021 when a magnitude Mw1,5 earthquake (most likely) took place in Fagradalsfjall mountain. The new fissure is expanding and but I am now estimating that the current length of the new fissure is 1,2 km based on Rúv News web camera view. The new fissure is north-east of the earlier eruption in Geldingadalir valley any.
The new fissure opening up. Copyright of this image belongs to Rúv. From Rúv web camera.
I’ll post update about this later today when I know more.
Update at 16:29 UTC
The larger fissure is around 300 meters long according to reports. Part of it seems to be under its own lava flow based on what I am seeing on new videos of the fissure. The second fissure is about 10 to 30 meters long. There is also a one single eruption vent in the area just outside of the fissure areas. The lava flow is going into Meradalir below the new fissures. It might soon go into a what seems to be a lake or a dried up lake in that valley that is a lot larger and deeper than Geldingadalir valley that is now full of lava. The eruption in the original craters continues but at lot less energy levels than before. This might only be temporary change but it is impossible to know for sure what is going to happen.
Next update is going to be again in few hours as this situation develops.
Pictures are from Department of Civil Protection and Emergency Management.
The eruption from a helicopter as seen today. Picture is from Department of Civil Protection and Emergency Management. Free to use.The lava river into Meradalir valley. Picture is from Department of Civil Protection and Emergency Management. The pictures is free to use.
During the night 4-April-2021 at 02:04 UTC an earthquake with magnitude Mw3,0 at 5,7 km depth took place 1,5 km south-west of Keilir mountain. This earthquake was felt in Reykjavík area and outside of it. Based on the earthquake location it looks like it is located in the dyke or close to it. This is part of the Krýsuvík-Trölladyngja volcano.
Earthquake activity on Reykjanes peninsula. Copyright of this image belongs to Icelandic Met Office.
Along the magma dyke there seems to be forming focused points of earthquake activity. Currently I am seeing two location. The first location is around the eruption in Geldingadalir valley (former) and the second location that seems to be forming is just south of Keilir mountain. It has been my experience during the eruptions over the last few years that this type of earthquake activity might suggests that new location where eruptions might take place based on this earthquake activity. It is impossible to know if anything is going to happen. There is no change in GPS data since the eruption started. The GPS data can be viewed here.
This is a short update of the activity in the eruption in Geldingadalir valley (former, as the valley has now filled up with lava or close to being filled with lava). The eruption is taking place in Krýsuvík-Trölladyngja volcano system. The eruption has been stable all week. On Sunday 28-March-2021 other side of the craters that had built up collapsed into the lava stream that has formed below the erupting craters. Both craters are now about equal erupting size.
The lava that is now erupting is primitive Tholeiitic magma based on the chemical analyse from University of Iceland. That report can be found here (pdf).
Both craters are unstable and often suffer a collapse and rock slides and that often changes their look suddenly and drastically in a moment.
Icelanders continue to act like idiots in front of the web cameras that show the eruption online (I think all of them). The Rúv web camera is a large structure there that is easy to avoid (with solar panels and everything).
Lava boiling is a common occurrence that often breaks up through the newly formed crust in the new lava field. This happens without warning and often reshapes the lava field in a instance.
Spatter activity in the eruption craters often drops but the flow of lava seems to be stable based on the web cameras and observation reported in the news by volcano scientists according to the latest news I was able to find.
It is unclear when lava is going to start flowing out of Geldingadalir valley (former). It might start to happen this weekend or by next week.
Based on what I am observing on the web cameras at the writing of this article. A collapse might happen in the erupting crater on the right side on the screen (I don’t know what is north and south on the web camera). When that or if that happens is impossible to know, but the whole structure that I am seeing doesn’t look that stable when I write this article.
At the writing of this article a large collapse took place in the erupting crater on the left side on the camera. Resulting in block of the erupting vent and resulting in a lot of spatter activity as a result as it clears it self of the rock that fell into it.
Currently there are no signs of this eruption about to end. This eruption might go on for a long time. Next update about the eruption in Geldingadalir valley (former) should be on 9-April-2021 unless something major happens in the eruption.
Update 14:12 UTC on 3-April-2021
The eruption craters at 13:56 UTC on 3-April-2021. Copyright of this image belongs to Rúv. From Rúv YouTube stream of the eruption.
There is now in the northern crater (right side on screen?) a small lava fall. Its not big but it is few meters high. There are variations in spatter activity and the whole crater structure remains unstable. There are many collapses and changes now over one day.
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Yesterday (1-April-2021) an earthquake swarm took place east of Grímsey island. The largest earthquakes in this swarm had a magnitude of Mw3,8 and Mw3,6 and where possibly felt even if that was not reported. Total of 142 earthquakes have taken place when this article is written.
Earthquake activity east of Grímsey island. Copyright of this image belongs to Icelandic Met Office.
Earthquake activity is very common in this part of the Tjörnes Fracture Zone and it is now just around one year since a large earthquake swarm took place far west of Grímsey island in June 2020. It is difficult to know of more earthquake activity is going to happen at this location in next few days.
This is a short update on the situation about the eruption on 27-March-2021. This eruption is now classified as to be happening in Krýsuvík volcano system.
The eruption seems to be slowly increasing. The small craters on the left (on the web camera) have now merged into one larger crater. It is possible that the two remaining craters might merge into one large crater.
The magma fro this eruption is coming from 17 – 20 km depth and that can result in a eruption that can last a long time.
Geldingadalir valley is now almost filled with lava. It is expected to overflow by Easter in about 6 days based on current eruption rate of the lava.
Lake of lava has formed in the Geldingadalir valley. Videos have been posted on Facebook and other social media showing how dangerous the lava field currently is. Do not walk on the fresh lava. It is going to take decades and possibly centuries to cool down to a safe level.
The lava at it thickest is estimated now to be 20 to 30 meters deep.
There are fluctuations in the eruptions. Sometimes its slightly more and sometimes slightly less based on observations with the web camera on Rúv.
It seems that a mountain is being built by this eruption. How that is going to progress is difficult to know for sure.
In general there has not been a lot of change in the eruption since it started a week ago (19-March-2021). Next update is going to be hopefully on 2-April-2021 unless something major happens in this eruption.
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