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- #281
Well this interesting -- a swarm of mild but stronger than usual quakes in the Eldey system and a 1-pointer -- west of Grindavik.
This zoom shows you where things are relative to Grindavik (almost all of the Eldey system is underwater):
<Layperson speculation> I don't know what it means, but IMO did note in their update today that over 13 million cubic meters of magma is under Svartsengi now and inflation continues.
That is way more than what triggered the last two eruptions, so magmatic pressure can't be working alone here.
I wonder if that "holding force(s)" might be weakest west of Svartsengi (Eldvorp and Eldey, basically, since it's affecting the southern part of this region).
I don't see Eldvorp in the Catalogue of Icelandic Volcanoes online, although volcanologist Armann and Dr. Wikipedia talk about it. So I'm not going to speculate about that at all.
Those eastward-centered quakes in the Eldey swarm shown might be interesting, if we could see them relative to the November 10th dike.
I haven't seen any graphics about the submarine extension of that dike.
It did continue out there, though, and while it's unlikely that it and whatever is going on at Eldey could be connected (given the strong SW-NE tectonic trend here), this general offshore area south and west of Grindavik might get interesting.
Of note, the most recent activity on land did seem closer to Grindavik (as mentioned in earlier post), but the boffins writing the IMO geoscientist notes attribute this to magma cooling.
We'll just have to wait and see.
I hope that the Svartsengi sill magma does migrate westward before coming to the surface again -- there are fewer people and less infrastructure on the peninsula tip.
Tourists and the wildlife they come to watch can just drive/fly/swim away from trouble.
Iceland is gorgeous, isn't it.
There was a swarm here a few weeks ago and IMO installed a GPS -- on that one large island there, possibly.
Perhaps we'll get some news about that in the next few updates.</layperson speculation>
This zoom shows you where things are relative to Grindavik (almost all of the Eldey system is underwater):
<Layperson speculation> I don't know what it means, but IMO did note in their update today that over 13 million cubic meters of magma is under Svartsengi now and inflation continues.
That is way more than what triggered the last two eruptions, so magmatic pressure can't be working alone here.
I wonder if that "holding force(s)" might be weakest west of Svartsengi (Eldvorp and Eldey, basically, since it's affecting the southern part of this region).
I don't see Eldvorp in the Catalogue of Icelandic Volcanoes online, although volcanologist Armann and Dr. Wikipedia talk about it. So I'm not going to speculate about that at all.
Those eastward-centered quakes in the Eldey swarm shown might be interesting, if we could see them relative to the November 10th dike.
I haven't seen any graphics about the submarine extension of that dike.
It did continue out there, though, and while it's unlikely that it and whatever is going on at Eldey could be connected (given the strong SW-NE tectonic trend here), this general offshore area south and west of Grindavik might get interesting.
Of note, the most recent activity on land did seem closer to Grindavik (as mentioned in earlier post), but the boffins writing the IMO geoscientist notes attribute this to magma cooling.
We'll just have to wait and see.
I hope that the Svartsengi sill magma does migrate westward before coming to the surface again -- there are fewer people and less infrastructure on the peninsula tip.
Tourists and the wildlife they come to watch can just drive/fly/swim away from trouble.
Iceland is gorgeous, isn't it.
There was a swarm here a few weeks ago and IMO installed a GPS -- on that one large island there, possibly.
Perhaps we'll get some news about that in the next few updates.</layperson speculation>