Today (21-July-2021) few deep earthquakes took place in Fagradalsfjall mountain that is part of Krýsuvík-Trölladyngja volcano system.
This earthquake activity was not big and the largest magnitude recorded was a magnitude of Mw0,8. Most depth that appeared had a depth of 13,4km.
It is difficult to know what this means. What is possibly happening is that more magma is pushing up in the magma feeding that now exist where the eruption has been happening. If that is happening, it can result in new craters or fissure opening up and start erupting. At the writing of this article this earthquake activity seems to be ongoing, but at slow rate and small earthquakes only so far.
Fog continues to block view to the crater and Fagradalsfjall mountain. But harmonic tremor data shows that the Fagradalsfjall mountain eruption is currently not erupting.
There has not been a lot of change in the eruption during this week (28-May to 5-June) in the eruption of Fagradalsfjall mountain that might be part of Krýsuvík-Trölladyngja volcano system.
The crater continues to get bigger. The crater grows by collapsing on the inside and expanding it walls following that it seems. Current height of the crater is 300 to 500 meters. This is a bad estimate based on web camera views.
The main viewing area is now cut off from walking people because lava has flowed over the lowest point on the walking path.
There is now a risk because of the overflow over the walking path that the western barrier is going to be breached soon.
In general the lava doesn’t travel far but it builds up close to the erupting crater and is now at locations hundreds of meters thick.
If the eruption continues as it has been doing the whole area is going to go under lava in next 6 to 10 months. As the lava just keeps building up.
There are no signs that this eruption is ending.
There are no other news about this eruption that I know of. It continues as it has been doing since 19-March-2021. In other parts of Iceland it has also been quiet or minimal activity not worthy of reporting.
This article is a little late because I was dealing with headache issue for the last 12 hours.
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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 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.
This is a short article on the activity in Fagradalsfjall volcano. This situation is developing quickly and it is impossible to know what happens next.
During the night of 9-March-2021 from 05:20 UTC until around 07:00 UTC an harmonic tremor pulse was detected by Icelandic Met Office. This shows that the magma is still expanding into the Earth crust below Fagradalsfjall mountain and according to Icelandic Met Office it looks like the dyke is expanding in south direction but it is going to take a day or two to confirm that with GPS data.
There have been fewer stronger earthquakes in last few days. While the there are fewer strong earthquakes the amount of earthquakes has not really dropped in any number, most earthquakes are small in magnitude and only few reach magnitude above Mw3,0. This quiet period is not expected to last for any amount of time while magma continues to be injected into the crust of Fagradalsfjall volcano. There continues to be a high risk for earthquake with magnitude Mw6,0 to Mw6,5 along with risk of Mw6,5 earthquake in Brennisteinsfjöll volcano. Currently no magma movement is being detected in Reykjanes volcano, Krýsuvík volcano or Brennisteinsfjöll volcano.
Yesterday (01-May-2015) a minor dyke intrusion took place in Katla volcano. This dyke had depth down to 26,9 km and up to 18,5 km. This is the second dyke intrusion in this are in short space of time. Largest earthquake in the following earthquake swarm had the magnitude of 2,0.
Dyke intrusion in Katla volcano (dense cluster of earthquakes). Copyright of this image belongs to Icelandic Met Office.
While this doesn’t signal imminent eruption in Katla volcano this activity does have me concerned due to past experience with activity in Katla volcano. This might die out, but there is no way to know for sure. All that can be done is to wait and see what happens next in Katla volcano.
Notice on Grímsfjall volcano
There has been a slight increase in earthquakes in Grímsfjall volcano. This suggest that the volcano is about to be ready for its next eruption. Earlier eruptions took place 2011, 2004, 1998 … etc. It is impossible to know when or how big next eruption in Grímsfjall volcano is going to be.
Today (27-February-2015) there was no visible lava flow from the main crater in Holuhraun. The eruption is not officially over, this however seems to be the end of this eruption in Bárðarbunga volcano. It appears that gas emission continue from the crater and Holuhraun at the moment, it can be expected those are going to end in next few weeks to months.
New video of the crater in Holuhraun can be found here.
This update is going to be slightly shorter than usual because I am sick (I got flu at the moment).
Over the past two weeks there has been considerable drop in the lava lake.
Lavafall was seen on new images (in the one of the lava rivers) in Holuhraun yesterday (05-February-2015).
Earthquake activity in Bárðarbunga volcano continues to drop. It continues to be classified as considerable.
GPS data show that the area around Bárðarbunga volcano continues to subside towards the volcano.
The eruption in Holuhraun might end in 5 – 12 months, there is also a chance it might go on for years at low level. There is no way to know for sure.
Sulfur dioxide pollution continues to be a problem in Iceland. Depending on wind direction. Current release of Sulfur dioxide from the eruption in Holuhraun is from 30.000 tons/day and up to 80.000 tons/day.
Earthquake activity in Bárðarbunga volcano for the last 48 hours. Copyright of this image belongs to Icelandic Met Office.
Largest earthquake in the past 48 hours was a magnitude 4,9 earthquake in north-east Bárðarbunga volcano. It has now been one month since magnitude 5,0 or larger earthquake took place in Bárðarbunga volcano.
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Since last update nothing major has changed in Holuhraun. There have been some changes in Bárðarbunga volcano it self and I am going to cover that later in this article. The magma flow from the craters in Holuhraun remains high at the moment, with latest flow measurements saying that flow of lava is now 100m³/sec. There seems to be uncertain or maybe changes in the flow of lava out of the crater. The volume is now ~1,4 km³. The lava-field has been getting thicker over the past weeks and closest to the craters it is now around 40 meters thick. New estimate of when the eruption might end are now 4 to 15 months.
Earthquake activity in Bárðarbunga volcano for the last 48 hours. Copyright of this image belongs to Icelandic Met Office.
Earthquake activity remains high, but it continues to drop at steady rate between weeks. Earthquake activity now also drops between peaks in activity. I still don’t know if a small eruption took place in Bárðarbunga volcano. Nothing has yet been confirmed and it might remain unconfirmed for a long time. I am also seeing small spikes in the harmonic tremor data due to hydrothermal activity in Bárðarbunga volcano (far as I can tell).
If anything major happens I am going to post update about it soon as I can.
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Nothing major is to report from last update on Holuhraun eruption. It continues at the same phase as before. It has been slowly diminishing over the past few weeks and continues to do so. There are complex reasons for this, but one thing is clear. This eruption is going to end one day. The size of the lava is unclear that the moment. It volume is now around 1,4 km³ according to the news. Cauldrons in the glacier, on top of the Bárðarbunga volcano caldera rim have been getting deeper over the past few weeks. This means that the hydrothermal activity in those areas is increasing and presence of magma at shallow depth. This also suggests that amount of magma at that shallow depth is increasing. If it is going to erupt is unclear at the moment, there are however currently higher chance that it is going to do so, rather than not.
Earthquake activity in Bárðarbunga volcano for the past 48 hours. Copyright of this image belongs to Icelandic Met Office.
There has been less earthquake activity taking place for the past 48 hours then during same days last week. There are peaks and lows in the earthquake activity, there might be a lot of earthquakes taking place one day, other days there appears to be a low in earthquake activity. What is also playing in as a factor here is the fact that bad weather has been taking place in Iceland for the past few days.
Last week scientists have been doing studies into the gas content of the eruption to see what is contains. SO² continues to be a problem in Iceland, depending on wind direction.
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Article updated at 22:53 UTC. Article updated at 22:55 UTC.
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