This is a short update. Information there might go outdated quickly and without warning. This article is written on Wednesday 22. November 2023 at 21:32 UTC.
There’s little news to report at this moment. Mostly because of bad weather. The progress of the dyke has also stalled from earlier, or this might be it for now. It is difficult be sure currently.
The inflation at Svartsengi (upwards movement) stopped in the last 24 hours. This either means this series of events is stopping for now or something major is about to happen. I am not sure. Risk of this being a error are small, but this might be interference from weather (rain, snow).
The air code for Reykjanes volcano has been downgraded to yellow.
The situation in Grindavík and in Sundhnúkagígar and the nearby area can still change without much warning. Since the ground is very fractured there and is not going to be much resistance to any magma movements in the near future.
If anything more happens. I’ll update soon as I can.
This is a short update on the situation in Grindavík. This article is written on 20. November 2023 at 22:22 UTC.
There’s a storm in Iceland until 23. November 2023. When the wind is going to start die down again. This means that Icelandic Met Office is going to record fewer earthquakes because strong ocean waves and wind.
There has not been much change since yesterday. This is normal.
Inflation in Svartsengi is up to 30mm/day and this is a increase, since inflation used to be around 15mm/day.
Since Friday 10. November 2023 the inflation in Svartsengi has been around 150mm over the last 11 day time period.
It took 17 days from start on October 25 of the magma inflow into the Svartsengi dyke until it broke on 10. November and the created the Sundhnúkar to Grindavík dyke.
It is a question what happens when next 17 days come up. Because whatever the hold is for the magma in the dyke in Svartsengi is going to break it is going to start the process as happened on 10. November 2023 and possibly into the current dyke, or possibly create a new dyke next to the current one (its a possibility, not a large one, but it is there).
There has not been a lot of information released today and I don’t see a lot on seismometers and other instruments around Grindavík town currently.
This type of quiet period before an eruption are common. Why is not well understood. Eruption might not happen, but it is not likely that nothing is going to happen in this. Both is magma too close too the surface and there’s too much inflow of magma into the dyke at Svartsengi. This is how I see the current situation.
If anything happens. I’ll post update soon as I can.
This is a short update on the activity in Grindavík on 19. November 2023. Information here might go out of date without warning. This article is written at 22:28 UTC.
This morning an earthquake with magnitude of Mw3,7 took place in Krýsuvík-Trölladyngja volcano. This earthquake was felt in Reykjavík area. This earthquake happens because of all the displacement that is now happening next to Grindavík town.
This is also an update for 18. November 2023. I was trying to get a little time off from writing.
Little has changed in last two days. Parts of Grindavík town continue to sink or rise depending on location. Most measured movements is around 25 cm last I did see. If that is correct today I am not sure.
Inflation in Svartsengi is around 130mm since Friday 10. November 2023 according to GPS measurements and satellite measurements.
Inflow of magma into Svartsengi is estimated to be around 50m3/sec when this article is written according to the news. Inflow of magma into the dyke was 75m3/sec or more few days ago. That has possibly changed to a lower number in last few days.
Earthquake activity remains about the same in the dyke. Around 800 to 2000 earthquakes a day along the 15 km long dyke.
It is impossible to know when this area is going to erupt. It can take up to three to four weeks to happen. It might be a shorter time period, it is impossible to know what happens when it comes to volcanoes and dyke activity.
If anything happens. I’ll post an update quickly as I can.
This is a short update on the situation in Grindavík on 17. November 2023. Information here can go outdated quickly and without warning.
Grindavík town continues to sink as the rift valley continues to move. The speed of sinking has slowed a little according to the news today.
Earthquake activity has slowed down in last few hours (this is written around 22:51 UTC). What that means is unclear.
Some houses in Grindavík town have been completely destroyed. Iceland has a natural disaster fund for this type of situation and that is going to cover the owners loss according to the news.
It took me a week. But it seems that this dyke intrusion under Grindavík town is because of the magma sill (dyke) under Svartsengi. That area has inflated around 110mm in a week. That is a inflation of 15mm/day based on my best calculations. That is a lot of inflation, since before 10. November the inflow of magma into Svartsengi was at most 8m3/sec according to measurements of Icelandic Met Office.
The sill in Svartsengi created a lateral dyke in Sundhnúkar and nearby areas. When the pressure in the sill is high enough again it is going to push the magma into the dyke at Sundhnúkar again with the same force as it did before. How long that takes I don’t know. Last time this was from 25. October to 10. November. That’s seventeen days, but there was a lot of deeper sills in Svartsengi and its impossible to know much, if anything flowed form them into the dyke. This is my personal view, it might be wrong. But this is what I am reading from the data.
Risk of the eruption remains high because there’s a ongoing inflation at Svartsengi. When a eruption starts is impossible to know.
If anything happens. I’ll post update soon as I can.
This is a short update on what is happening in Grindavík on 16. November 2023. Information here can go outdated quickly and without warning.
The situation is mostly the same as yesterday (15. November 2023), but few things have happened and that is enough for me to publish this article.
Sulfur dioxide has been detected in a drilling hole in Svartsengi. This drilling hole is such that it end point is close to Hagafell mountain east to Svartsengi power plant. I think this might be a cold water hole. It has a depth of 2,5 km. This means that magma is at or close to that depth. Ground water in this area doesn’t go deeper than 1,9 to 3 km I think (I am not sure on how the fresh water ground level works in this area).
Eruption is expected from hours to day based on most recent measurements from Icelandic Met Office.
Grindavík town continues to sink according to news today (16. November 2023). Difference between days can be as much as 25 cm.
Mbl.is (Morgunblaðið) has a video of the damage done by this sinking on their website here. Its in Icelandic.
The situation for now is quiet, but that might only last for few hours to days longer before an eruption starts. Since earthquake activity strongly suggests that magma is looking for a way to the surface. While some magma is at shallow depth of 400 to 500 meters. There’s not enough of it to start an eruption. That can change without any warning at any time in this situation.
I’ll write updates if anything more happens here as quickly as I can.
This is a short update on what is happening in Grindavík on 15. November 2023. Information here might go outdated quickly.
In general, not much has changed since yesterday (14. November 2023).
There’s no change in earthquake activity. Strong wind in the Reykjanes peninsula might be masking some of the smaller earthquakes.
Part of the harbour area has started to sink according to news. I am not sure how much, but I think it might be considerable sink.
Speed of the sink in some areas of areas inside Grindavík has increased from 7 cm for each 24 hours to 12 cm for each 24 hours since yesterday. Some areas inside Grindavík have lowered as much as 2 meters or more.
Inflow of magma into the dyke continues to be at 75 m3/second according to news reports today. This is a lot of magma inflow into the dyke. The eruption in Holuhraun in 2014 and 2015 had an flow of 90 m3/sec when it was the most.
It is reported on mbl.is that it is now considered that magma might be flowing directly from the main magma chamber at 20 km to 40 km depth under this location in Reykjanes peninsula. That news is in Icelandic here.
Parts of Grindavík town has lost power, hot and cold water because of sinking of the ground and movements. Emergency repair is going to be attempted tomorrow if it is safe.
Eruption might happen at Sundhnúkar and Hagafell, where the highest flow of magma is happening according to Icelandic Met Office and the news.
Eruption at many craters at the same time is what is going happen here. Based on what I am seeing. That means more lava covering larger area quicker than the small eruptions in Geldingadalir, Meradalir and at Litli-Hrútur. Where it was just one crater and a small eruption.
Something is holding back the magma from reaching the surface. What that is unclear. But magma is at shallow 500 meters or less according to measurements done by Icelandic Met Office. This shallow depth means that magma can start erupting without much warning or notice in the dyke.
There is a chance that parts of Grindavík town might sink under the ocean because of the ground sinking. When eruption starts, what goes under lava depends on where the eruption is going to start and where the lava is going to flow. Both are random events that is impossible to know anything about.
If anything happens. I’ll post update soon as I can. If anything happens tomorrow I’ll write about it. Otherwise I plan on publishing next article on Friday 17. November 2023. Since changes at the moment are not that big changes between days currently.
The magma is at 400 meters depth, where it is at its most shallow. I am not sure on location, but I think it is just north-east of Grindavík town.
There is strong wind on Reykjanes peninsula. That normally hides some of the smaller earthquakes happening. Icelandic Met Office continues to record 700 to 3000 earthquakes each day. Most of them are along the dyke and most of them are in the magnitude range of Mw0,0 to Mw3,1. With the stronger ones happening least often.
Inflow of the magma into the dyke is at the writing of this article around 73 m3/s to 75 m3/s. On Friday 10. November that inflow was 1000 m3/s.
Sulfur dioxide was detected today north of Grindavík. That suggests that magma might be at shallow depth in the dyke area.
News reports today did say that the area in Grindavík and nearby continues to sink around 7 cm over 24 hour time period. This might be uneven process depending on the area.
Lakes south of Grindavík have been seen growing, as the area continues to sink and get lower. It is a question of parts of this area is going to get flooded by the ocean soon. This is reported on Facebook by Eldfjalla- og náttúruvárhópur Suðurlands.
The GPS station just north of Grindavík has lowered by 1400mm since Friday 10. November 2023. The stations on the east are going up, some much as 1 meter. While the GPS stations on the west side are lowering.
This situation changes quickly and often from hour to hour. I’ll post new updates if something major happens, quickly as I can.
Article updated on 15. November 2023 at 00:21 UTC. – Removed information that might not be correct.
This is a short update on the eruption in Fagradalsfjall mountain on 21-May-2021. This is part of the Krýsuvík-Trölladyngja volcano system.
There has not been a lot of change since last update on the eruption. The eruption has now been going on for two months and few more days. There are no signs of the eruption ending.
The lava fountain activity continues as it has been doing for the last month.
Output of lava has been increasing and is now around 11m3 compared to 5m3 at the start of the eruption.
Lava is now on its way to the ocean by flowing down into Nátthagadalur valley. There is an attempt to try and stop or delay that from happening by pushing up defences and try to hold back the lava field. It is my personal view that this attempt is going to fail, at most it is only going to delay the lava a little bit. Since the lava field also has to get over a hill that is in its path anyway. That is only going to take few days to a week depending on how much lava is being fed into this part of the lava field. That changes all the time with no warning.
Most of the lava goes into Meradalir valley where it is for now not putting anything in danger or risking infrastructure.
SO2 pollution is starting to show in south Iceland. There was also report of static electric charge build up around the eruption site yesterday (20-May-2021). It didn’t result in a lightning but the risk was in place for a good while.
There are for now no other news of the eruption and it has been quiet in other parts of the Iceland during the last week.
The eruption in Holuhraun ended yesterday (27-Februar-2015) it seems. Current status of Bárðarbunga volcano is now yellow. While the eruption is over the area continues to be closed for public due to danger of new eruptions in the area, both outside the glacier and inside it. It is unclear what is going to happen next in Bárðarbunga volcano. There is also a considerable gas emission from Holuhraun crater at the moment and that gas is toxic.
Current earthquake activity in Bárðarbunga volcano and for the past 48 hours. Copyright of this image belongs to Icelandic Met Office.
What happens next is not known. There is a high risk of new eruption taking place under the glacier. I don’t know if subsidence of the caldera is going on at the moment or has stopped. It might take days, weeks or months until inflation starts again in Bárðarbunga volcano. This is a rifting event and that means this is far from over. For the moment however it is going to be a little break (at least, it can be hope) in the activity in Holuhraun or Bárðarbunga volcano. The lava and the crater continue to be extremely hot (~800C) and are going to remain hot for many years (5 years?).
Since the eruption in Holuhraun is over I won’t post any update next Wednesday. Next update is going to be when something happens.
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.
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