Today (26. February 2024) at 18:27 UTC an earthquake with magnitude of Mw3,4 took place in Krýsuvík volcano. This earthquake was felt, but I don’t know over how wide area.
This earthquake activity might be connected to the inflation that is happening in Svartsengi volcano, as it changes the stress values in the crust over a large area. More earthquake activity is possible in this area.
I am sorry for slow updates. All this activity and eruptions keeps me busy with many things. I also needed a little break from writing articles.
According to Icelandic Met Office and what I’ve been seeing on GPS data from around Svartsengi volcano an eruption is expected possibly next week, it might happen earlier or later, there’s no way to be sure on this. But the inflation has reached the same level just before the eruption on 8. February 2024. What is going to happen in next eruption is impossible to know, until the eruption starts. There is ongoing risk that next eruption is going to happen closer to Grindavík town and not in Sundahnúkagígar area as the eruption on 8. February 2024 took place.
At the current rate, there’s going to be an eruption in Sundhnúkagígar area every 30 or so days until something changes. When that happens is impossible to know. This 30 day eruption cycle might go on for a long time, even many years.
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 morning (08. February 2024) at 06:02 UTC an eruption started close to Sundhnúkagígar, close to the area where the eruption started on 18. December 2023. The eruption fissure is at the writing of this around 3 km long, but the fissure is getting longer, based on views from web cameras.
This eruption is at favourable location. Since its far way at the moment from all buildings and infrastructure. That might change if the fissure stretches more to the south. This eruption started really quickly, according to Rúv, from the start of the earthquake swarm until the eruption started the time was only about 30 minutes. The time this took on 18. December 2023 was 60 minutes.
I’ll post more information later today when it is clear how this eruption is progressing.
Cookie acceptance
We use cookies on our website to give you the most relevant experience by remembering your preferences and repeat visits. By clicking “Accept”, you consent to the use of ALL the cookies.
This website uses cookies to improve your experience while you navigate through the website. Out of these cookies, the cookies that are categorized as necessary are stored on your browser as they are essential for the working of basic functionalities of the website. We also use third-party cookies that help us analyze and understand how you use this website. These cookies will be stored in your browser only with your consent. You also have the option to opt-out of these cookies. But opting out of some of these cookies may have an effect on your browsing experience.
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.
Functional cookies help to perform certain functionalities like sharing the content of the website on social media platforms, collect feedbacks, and other third-party features.
Performance cookies are used to understand and analyze the key performance indexes of the website which helps in delivering a better user experience for the visitors.
Analytical cookies are used to understand how visitors interact with the website. These cookies help provide information on metrics the number of visitors, bounce rate, traffic source, etc.
Advertisement cookies are used to provide visitors with relevant ads and marketing campaigns. These cookies track visitors across websites and collect information to provide customized ads.