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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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.
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.
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.
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.
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
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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This information is going to get outdated quickly. This article covers Krýsuvík-Trölladyngja volcano. This article is written on 21-March-2021 at at 00:40 UTC.
This eruption is tiny. The amount of magma erupted is now around 0.02km3 but this number might not be fully accurate since I’ve not seen any published number about of volume of lava erupted so far.
This is unconfirmed but it is possible that an new fissure opened up under the lava field next to the hill side (seen on the web camera, this is on the left side).
The current erupting fissure is now about 200 meters long and might be getting shorter.
Earthquake activity has almost stopped at the writing of this article.
This eruption might only last 1 to 3 days before it stops.
There is no sign of deflation in the GPS data at the writing of this article.
There are no other reports about this eruption at current time. This might change without warning.
Beint vefstreymi af eldgosinu – Vogastapi (Rúv.is) – Added 22-March-2021. View from a distance. Should show a red glow from the eruption if the weather isn’t too bad. – This web camera is no longer active!
Update at 15:28 UTC – One side of the main crater collapses
Here is a video of the main crater collapse on one side and give lava a new path for short period of time. At the writing of this update that path for the lava has closed down again.
Kvikustreymið braut sér nýja leið (Rúv.is) – This is a new video of the crater collapse that took place at 14:20 today (21-March-2021).
Article updated at 15:29 UTC. New information added. Article updated at 21:21 UTC. New information added. Article updated at 03:06 UTC on 22-March-2021. Web camera added.
em>Article updated at 16:34 UTC on 22-March-2021. Web camera has been removed by Rúv – comment added to that web camera.
This is a short overview of the eruption that is now ongoing in Geldingadalur in Fagradalsfjall mountain area. This is part of Krýsuvík-Trölladyngja volcano system according to latest information. This information might change as the time and more information is collected. This article is written on 20-March-2021 at 02:58 UTC.
This is the first eruption in Krýsuvík-Trölladyngja volcano system since the year 1340.
The eruption started at 20:45 UTC according to Icelandic Met Office. The harmonic tremor from the eruption is almost invisible.
The fissure is at the writing of this article estimated about to be 1 km long with the direction south-west and north-east.
Currently the eruption is small and there is no risk of damage to any infrastructure. Next road (currently closed because of earthquake damage) that might get damaged is 2,5 km distance from the eruption site.
This eruption suggests that more eruption might start in different fissures once this eruption is over.
The valley that the lava is flowing into might get filled with lava if the eruption lasts long enough. The valley next to it is equally deep so there is no danger of this lava flow.
The eruption is in a area that is difficult to access even by a car.
The eruption might only last for two to three days as it currently looks but that might change without warning since it is impossible to know for sure what is going to happen next with this eruption.
There are no good web cameras of this eruption since it is remote and started late on Friday night and the weather on Reykjanes peninsula is not good for today (20-March) or tomorrow (21-March).
Updated at 04:49 UTC. Web cameras added to this article.
Article updated at 03:49 UTC. Information added. Spell check fixes. Article updated at 04:52 UTC. Web cameras added. Article updated at 14:44 UTC. New web camera added from Rúv.
This is a short article written on 17-March-2021 at 17:49 UTC. The situation can change without warning.
It has been less activity in in Fagradalsfjall volcano (Krýsuvík volcano). Current day to day change is not a lot at the writing of this article but it is also possible that bad weather that is now passing over Iceland is masking some of the smaller earthquakes in the dyke between Keilir mountain and Fagradalsfjall mountain. Inflation continues at what seems to be about the same rate as yesterday (16-March-2021).
Number of strong earthquakes has dropped after the strong earthquake activity during last weekend (12 to 14 March). What also changed is that the dyke can’t move more south then it already has. It seems that it hit a impasse in the crust that it was unable to break or go around (harder crust is the most common why this happens). The current status is a waiting for the eruption to start and when that happens is impossible to know.
Since there is not a lot of change going on at the writing of this article I am going to slow down the number of updates I am posting. Next update is going to be when something happens or at the latest Monday 22-March 2021.
This is a short article because the situation is always changing. This article is written on 15-March-2021 at 21:23 UTC. This article is about Fagradalsfjall volcano but Icelandic Met Office updates go to Krýsuvík volcano so I link to that volcano also.
Between Friday and Monday the activity in Fagradalsfjall volcano was really strong. Several earthquakes with magnitude above Mw4,0 took place and the second largest earthquake took place on Sunday 14-March at 14:15 UTC with the magnitude of Mw5,4. Earlier that day at 12:34 UTC an magnitude Mw5,2 earthquake had taken place. According to the news (Icelandic) over 50.000 earthquakes have taken place since 24-February-2021 when this earthquake activity started (20 days ago). Of those six have been larger than magnitude 5, earthquakes with magnitude between 4 to 5 have been 53 and total of 524 earthquakes with magnitude between 3 to 4. Inflation is now reported to be 20 cm or 10 cm on both sides of the dyke. Eruption is expected to happen close to or in Nátthagi valley soon. When that happens is impossible to know but the magma inflow into the dyke doesn’t show any signs of slowing down or stopping.
It has also been reported that the magma dyke managed to push it self a little more south in the line it had been then compared to Friday according to newest data that scientists have access to. Today (15-March-2021) earthquake activity has been small and slow but after 16:30 UTC it started to increase again but at the writing of this article no major earthquake has happened. It has mostly been small earthquakes taking place.
If anything major happens I’ll post update soon as possible.
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This article is short because the situation is always changing. This is about the volcano Fagradalsfjall but I have also added Krýsuvík because that volcano is being updated at Global Volcanism Program website. I am not sure currently what volcano is considered active in this make injection. This article is written at 20:39 UTC.
Today (12-March-2021) at 07:43 UTC an earthquake with magnitude of Mw5,0 at 3,7 km depth took place close to Nátthagi valley just south of Fagradalsfjall mountain. Over the last 48 hours 72 earthquakes with magnitude above Mw3,0 have taken place. This earthquake activity is happening at the south end of the magma dyke that has now stopped moving south but continues to expand based on the earthquake activity that is now happening. This is also the location where an eruption might happen without any warning or strong earthquake activity. Eruption out on the ocean is no longer considered a possibility because the magma dyke stopped moving south.
GPS data shows that inflation remains heavy and has moved some GPS stations up to 120mm over a time period of two weeks. There are no signs of this inflation stopping or slowing down.
Next article is going to be on Monday 15-March-2021 if an eruption doesn’t happen or something else major doesn’t happen. I am hoping to get weekend break this weekend. If that is going to be successful is currently unclear.
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