Posted on by Jón Frímann

Update on the eruption at Litli-Hrútur on 11th July 2023 at 17:18 UTC

This article is short. The eruption is mostly stable at the writing of this article but the situation can change quickly without warning.

  • The eruption has changed in last few hours. It seems to be in only one crater that is slowly forming. The eruption has stopped at the north most end of the eruption fissure. At the writing of this article.
  • The dyke now extends 1 km under Keilir mountain in the direction of north-east. This might be a new dyke intrusion and not connected to the dyke that started the current eruption. This might result in a second eruption soon, but its too early to know for sure at the writing of this article.
  • The eruption started large fires in the moss and other plants in this area around Litli-Hrútur. This has resulted in massive toxic smoke in this area.
  • There’s a high risk of the volcano gas from the eruption, along with the toxic smoke from all the plants and moss burning.
  • Interestingly, while earthquake activity has dropped it has not stopped. Why that has happened is a bit of a mystery, it might be connected to the possible new dyke that has formed under Keilir mountain.
  • Yesterday (10. July 2023) the longest the fissure extent was at 1500 meters or 1,5 km. Since then it has gone down to one erupting crater that seems to be 50 meters to 100 meters long.
Map of the magma dyke and the eruption fissures on a map from Icelandic Met Office and others. Orange area between Keilir and to Meradalir valley show the danger area around the eruption area.
Map of the danger area around the eruption. The orange area is the danger zone that people should not travel over. Copyright of this image belongs to Icelandic Met Office and others.

 

It is impossible to know how long this eruption is going to last. Since dyke intrusions are poor magma containers this eruption might be a short one if there isn’t a constant supply of fresh magma from the deep mantle. Its too early to know if that is the case here. I have also noticed that once the eruption ends in any area, that area is not going to erupt again. When the eruption ends, it ends forever and that makes this a single eruption activity or crater rows. This area might be Monogenetic volcanic field (Wikipedia).

Since this type of eruptions are mostly uneventful and just continue. I plan on only posting updates when there are some news or changes to the eruption happen.

Update at 17:41 UTC

ISOR is reporting that their station called FAF (Fagradalsfjall) has to be moved because the lava is flowing directly at it. They are going to find a new location for this station. This report can be seen here on Facebook in Icelandic.

6 Replies to “Update on the eruption at Litli-Hrútur on 11th July 2023 at 17:18 UTC”

  1. Is there a glossary where for instance can be read what a dyke intrusion exact is?

  2. I was just watching the north RUV feed and literally the whole side of the volcano collapsed. It was wild to see.

    1. It clearly was a large flow event. According to experts this is something that can happen in this type of eruption.

      I wonder how long it is going to take the eruption to re-build the crater and close this collapse and get the flow south again.

  3. The flow from the colapsed side already started flowing to the south. So, two flows …

  4. The original flow has stopped. The flow is now from a large lava pond that has formed. The flow is going south for now in the same direction as original flow.

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