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.
This is a short article about the eruption in Fagradalsfjall mountain that is part of Krýsuvík-Trölladyngja volcano system.
This week has been busy and please read the older articles about what happened earlier in this week.
Lava output is now 50% more according to University of Iceland measurements compared to start of the eruption (19-March-2021). Gas output is also more then in start of the eruption. It has resulted in problems depending on wind direction.
There is a high risk that an eruption might start south of Geldingadalir valley eruption. There is also a high risk that new eruption is going to start north of the 5-April-2021 eruption.
There is no change in inflation in the area. It has slowed down but remains the same.
There continues to be low level earthquake activity along the dyke from Keili to Fagradalsfjall mountain.
Any change that is going to happen without warning and might not happen without any earthquake or little earthquake activity.
Next update is going to be on 16-April-2021 unless something major happens. This eruption is always changing and this weekend and next week might get interesting. If anything happens I am going to write new article soon as possible.
Update at 22:43 UTC
Icelandic Met Office released this map and press release (in Icelandic only) about the risk new fissures can open up both north and south the the current craters that are erupting. This page is updated regularly so if you are looking at this later than 9 to 10 April 2021 you might have to look for this information.
The map shows the area that is now at risk of new fissures opening up without warning.
Update 10-April-2021 at 15:20 UTC
Around 03:14 UTC on 10-April-2021 fissure number 4 did open up between fissure number 2 (5-April-2021) and fissure number 3. The eruption from this crater doesn’t seem to be large but it did happen under a new lava that had flowed over that same area few days before from fissure 2. In fissure/crater 1 the amount of erupting lava did drop a little just before the new eruption.
I am noticing that it seems new fissures are opening up more frequently then before. This seems to have changed after opening up of fissure 3.
Timeline of fissure openings so far.
1st fissure 19-March-2021
2nd fissure opened 5-April-2021
3rd fissure opened 7-April-2021
4th fissure opened 10-April-2021
Time period between new fissures opening up currently seems to be 3 to 4 days. I suspect that this is going to change soon and it is possible that new fissure that opens up might get larger as the eruption goes on. There seems to be phase in this eruption that is happening in Fagradalsfjall mountain. I am not perfectly sure what that phase is now since I’ve never seen this before and I don’t have any data on this type of eruption behaviour from other volcanoes outside of Iceland. That I know of.
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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I have now added Cloudflare to this website. That should prevent any problem with using it when a large spike in traffic happens as was the case when the eruption in Geldingadalir valley first started.
I re-applied to Amazon Associate accounts and that is now active but my website has to make a sale in next 180 days to make that permanent again. This rule also applies to old accounts. If you shop from Amazon using the Amazon banners (United Kingdom, United States, Germany) gives me a little extra income.
This is a short article about the eruption in Geldingadalur. The volcano that is erupting continues to be Krýsuvík-Trölladyngja volcano system. This might change at later date. This article is written on 22-March-2021 at 17:30 UTC.
The eruption is now mostly just in one crater. There is some activity in two other craters but it seems to be getting smaller as the eruption goes on.
This eruption is tiny and one of the smallest eruption observed in Iceland.
There is risk of new eruption opening up once this eruption ends or starts to get close to ending.
There is a fissure in the ground on the right side of the main crater (as seen on the web camera). A lot of volcanic gas comes from that fissure but no eruption has taken place so far.
There has not been any noticeable deflation according to GPS data from today (22-March-2021).
The main crater is now estimated to be 30 meters high but it is unstable and collapses often.
The lava is estimated going to fill Geldingadalur valley in 10 to 14 days if the eruption continues this long.
Earthquake activity has almost stopped on Reykjanes peninsula after the eruption started. Once the eruption stops earthquake activity might increase again.
The last eruption period on Reykjanes peninsula lasted from the ~700 to the year ~1400. It can be estimated that current eruption period that has now started on Reykjanes peninsula is going to last until the year ~2400 to the year ~2600. During this time shortest time between eruptions is 1 year but the longest time between eruptions might be up to 10 years. How this going to be exactly is a big question but this estimate of mine is based on the limited historical data that I have read somewhere (I no longer remember where that was).
According to the evening news on Rúv the lava and magma that is now flowing into the valley of Geldingadalur is around 1200C and is a primitive magma of Tholeiitic magma series (Wikipedia). The source of this eruption is a magma chamber with the depths of 17 km to 20 km and the origins of the magma it self is far deeper into the hotspot below Iceland. This magma has a lot of CO and CO2 gases that are highly dangerous. There is also a lot of SO2 gas in the eruption and that is dangerous gas.
News in Icelandic about this
Since the eruption is now in stable activity I am going to limit update to if anything major happens. Next update about the eruption should be on Friday 26-March-2021. Other activity in Iceland is going to be reported as normal if anything happens.
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Article updated at 18:32 UTC. New web camera added. Article updated at 20:50 UTC. Web camera information updated. Article updated at 23:57 UTC. Information added about the eruption.
At 04:30 this morning (19-March-2021) an earthquake swarm started just off the coast of Reykjanestá. This activity looks tectonic in nature for now but it is highly focused in one location. This earthquake activity did start on 24-February-2021 when the Mw5,7 earthquake happened. This activity was only going on for short period of time on 24-February-2021 before it stopped until now.
Largest earthquakes in this swarm had a magnitude of Mw3,7 but in total of 10 earthquakes with magnitude above 3 took place in this earthquake swarm. Around 100 earthquakes where recorded at the writing of this article but after 06:00 this earthquake swarm slowed down from its peak activity around 05:50. This earthquake swarm might increase again without warning.
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 update on activity in Fagradalsfjall volcano. This is mostly on the activity on 6-March-2021.
Overview of current activity
Earthquake activity is mostly limited to small earthquakes.
Risk of eruption has not been reduced with current change in activity.
The magma dyke is at the shallowest on 2 km but it has an average depth of 5 km to 8 km depth.
Most of earthquake activity is closest to Fagradalsfjall mountain (north end?). The dyke is situated between Fagradalsfjall mountain and Keilir mountain.
Fagradalsfjall volcano has not erupted in last 12000 years.
There has not been any magma activity observed in Krýsuvík volcano and Reykjanes volcano (Svartsengi volcano?). All earthquake activity in those volcanoes are due to crust stress changes due to inflation from Fagradalsfjall volcano.
There remains a high risk of a strong earthquake with magnitude between Mw6,0 to Mw6,5 because of crustal stress changes that are connected to all the inflation that is now taking place in Fagradalsfjall volcano.
Harmonic tremor has not been detected again since Wednesday but that might change without warning.
Current web cameras of Keilir mountain and possible eruption area
This is a short update since this situation is developing quickly.
No eruption has started at the writing of this article. Harmonic tremor is slightly lower compared to when it started at 14:20 UTC in Krýsuvík volcano. This drop in harmonic tremor started around 16:00 UTC. This harmonic tremor is ongoing as for writing of this article. There are no signs of the rift valley formation on the surface yet, but it does show up on measurements, both GPS and satellite measurements. Earthquake activity is high at the writing of this article but most earthquakes are small in magnitude but there are few earthquakes with magnitude of Mw3,0.
Web cameras of the possible eruption area can be found in this locations.
Yesterday (29-August-2020) an ongoing earthquake swarm in Krýsuvík volcano or in the Reykjanes volcano increased. I am unclear what volcano system is responsible for this earthquake activity. It might be both volcanoes and if that is case it complicates matter.
The earthquake activity yesterday close to Krýsuvík or in Krýsuvík volcano. Used with permission and copyright of this image belongs to Icelandic Met Office.
Largest earthquake in this swarm had a magnitude of Mw3,6 at 19:06 UTC and the second largest earthquake had a magnitude of Mw3,4 at 16:23 UTC. Two earthquakes with magnitude MW3,0 also took place. The strongest earthquakes where felt in Reykjavík and other nearby towns. This earthquake activity is part of the activity that started in January in Reykjanes volcano and has been ongoing since then. Its has moved a little east in recent months and I am unclear on why that is exactly. There are no clear signs that magma is moving at the writing of this article to the surface.
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Today (6-July-2020) was an earthquake with the magnitude of Mw3,5 at 18:35 UTC in Tjörnes Fracture Zone an earthquake with magnitude Mw3,2 took place at 15:40 UTC. It is possible that this earthquakes was felt. This earthquake swarm started on 19-June-2020 and has been going on for three weeks now.
Ongoing earthquake swarm in Tjörnes Fracture Zone. Copyright of this image belongs to Icelandic Met Office.
There continues to be a risk for a earthquake with magnitude Mw6,0 to Mw7,2. There are no sign that this earthquake swarm is about to stop. It drops every hours to days before increasing again.
Please remember to support me with donations. It helps me with July. While I am mostly out of my money problems minor issues remain over July and maybe and August (I hope not). Thanks for the support. 🙂
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