This is a short update on the eruption at Sundhnúkagígar.
Four hour GPS data shows that inflation has already started in Svartsengi volcano, that is currently erupting. This inflation seems to have started soon as the eruption started to get lower around 13:00 UTC.
The lava flow damaged the hot water pipe from Svartsengi power plant and now around 26.000 people on the Reykjanes peninsula are without hot water. There is also some damage to the power infrastructure, but that is minimal and that power has been restored on the power lines that are next to the lava flow. The situation on the cold water is unclear, but it was at risk of damage.
This eruption was larger compared to the eruptions on 18. December 2023 and on 14. January 2024.
Small ash cloud formed today and the reason for that, according to experts in the news. Was that the eruption in part of the fissured ended so suddenly with a pressure drop that the fissure walls collapsed, allow ground to get in touch with lava and then ground water started to flow on the lava. Resulting in two clouds, one dark and a steam cloud. This was large for an about hour or two. Steam cloud was ongoing at writing of this article, but darkness prevents me from seeing if this has stopped. It is likely though.
The eruption is ongoing in two to three craters at the writing of this article.
It is expected, based on current rate of how much the eruption is slowing down that it is going to end tomorrow, 9. February or on 10. February.
Next eruption is going to be in March around 6th to 18th March if current pattern holds for Svartsengi volcano. There’s nothing to rule out that a new eruption might happen sooner. It is impossible to know what happens next in Svartsengi volcano eruptions.
If anything more happens. I’ll post update soon as I can.
This is a short update and information here might go outdated quickly and without warning.
This eruption is a short one and that’s how eruptions in Iceland are normally. This eruption might end by Friday to Monday, depending on what happens.
The flow from the craters that are erupting is around 10m3/sec. This is low compared to the start of the eruption on Monday 18. December 2023 and suggest that this eruption is going to end soon.
GPS data shows that Svartsengi volcano has only lowered around 80mm since Monday. This means there’s a lot of lava in Svartsengi for new eruptions to happen without much warning.
Earthquake activity along the fault valley has resumed, after stopping soon after the main eruption took place. This is interesting and I am unclear what this means at the writing of this article.
Icelandic Met Office is reporting that the eruption, even is small, is stable at the writing of this article. This can change without warning.
The lava field is now, according to best measurements around 3,7 km2 (square kilometres).
According to University of Iceland Earth science department, the chemical makeup of the lava shows that its more evolved in part than the lava in Fagradalsfjall volcano. This can be read here (new link, now in English). This means that this magma stopped on its way to the surface and cooled a little and changed chemical makeup before erupting.
This new lava is different than the lava that erupted 2400 years ago at the same location. Why that is I don’t know. It is going to take few years to maybe get an answer to this question when the experts have done their research and published their science papers.
It is interesting to see that Þorbjörn mountain continues to get lower, based on GPS data from today (20. December 2023). Icelandic Met Office has released new danger map and that can be found here in English on Icelandic Met Office website.
This is all the information I know of today (20. December 2023). Next article should be tomorrow (21. December), unless something happens then I’ll try and write article soon as I can.
This is a short update and information here might go outdated quickly. This article is written on 19. December 2023 at 21:46 UTC.
I am trying to collect and read all the information I can find. I don’t have access to everything my self, so I am depended on news and reports from Icelandic Met Office and others on what is happening in this eruptions. This is not unusual and has always been like this.
The eruption is now in 2 to 4 vents. I am little unclear at the writing of this article now many are erupting.
The new dyke seems to go into the dyke from 10. November. This can result in reactivation of the dyke from 10. November and result in an eruption along it, all 15 km at random location.
Current flow seems be around 50m3/sec at the writing of this article. I’ve been hearing that highest flow yesterday (18. December) was around 800m3/sec, but that number is for me unconfirmed. It dropped to 100 – 500m3/sec soon after the eruption started.
Early GPS data from today seems to suggest that Svartsengi volcano has lowered about 50mm since the start of the eruption. I am waiting for new GPS data on Icelandic Met Office website. That data hopefully shows up tomorrow (20. December).
There’s a lot of uncertain things that can happen with this eruption at the moment. Since there’s a lot of lava in Svartsengi volcano that has not erupted so far. New inflow of lava from the deep mantle is also a possibility and those can happen without warning as the pressure drops in Svartsengi volcano sill (or magma chamber).
I’ll post next update tomorrow (20. December 2023) or sooner if anything happens.
This article is short and is written at 16:10 UTC on 19. December 2023. Information here can go outdated quickly and without warning.
There has been a reduction in the eruption since it started at 22:17 UTC on 18. December 2023. This was to be expected. Since the eruption seems to be coming from a small sill in Svartsengi volcano, rather than a large magma chamber.
The eruption is now limited to three to four eruption vents. The largest one is where the eruption started. Crater building is ongoing.
The lava is flowing towards Fagradalsfjall volcano (mountain) at the writing of this article. This area is empty, outside of the the parking lots south of Fagradalsfjall. They are not at risk for now.
The problem with eruptions of this type is that they can grow again in size if different sill breaks and starts flowing into the established flow channels that magma is now flowing and creating the eruption. If that happens is impossible to know. This can also result in a eruption that goes on for a long time. If that happens, an lava might end up reaching far away areas.
It is going to take few days for GPS data to show what sill is deflating in Svartsengi volcano and what is going on in the crust in Svartsengi volcano.
Weather might be a problem for next few days on Reykjanes peninsula.
This area is not to hike around on. Its dangerous and the weather makes difficult walk extremely difficult. Just watch the online web cameras.
The lava field is large and it creates its own strong wind as the lava warms up the air around it. That can be difficult to deal with in the snow for anyone close the the eruption.
The dyke is longer than the part that erupted according to the news and measurements. The dyke is more south and it ends just 1,5 km north of Grindavík town. That area can erupt without warning if pressure starts to build up in that part of the dyke. That same goes for the north part of the dyke, how far more north the dyke is I don’t know.
I’ll post next update when I have more information what is going on or sooner if anything happens.
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.
Necessary cookies are absolutely essential for the website to function properly. This category only includes cookies that ensures basic functionalities and security features of the website. These cookies do not store any personal information.