It could be worth considering this... (TLDR: this might be the onset of a new eruptive episode on the peninsula which could last a few centuries).
Dr. Judith Hubbard (@JudithGeology)
Today, I am reading Caracciolo et al. (2023): https://doi.org/10.1016/j.epsl.2023.118378 In the "Reykjanes Peninsula ... there have been three 400-500 years long eruptive cycles in the last 4000 years at time intervals of about 800 years." The last cycle is illustrated in their Fig 1 and... 1/nitter.woodland.cafe
maybe a (short) move eastwards ?Yeah that sort of backdrop is why theres not much optimism about the viability of the town moving forwards.
I wonder if they might have another search, if the eruption / 'quake swarm subsides ?The (extensive) search was called off after 3 days - unfortunately he is still missing, presumed dead.
Good Grief !They conducted a fairly thorough search (100+ persons), at great risk to themselves, including opening up the fissure, then survey use of 3D scanning and a mini submarine. It looks likely that he fell into an underground river (the fissure was even larger than it appeared, dropping to groundwater levels, which were deep enough to exhibit tidal influence). Quite possibly he was subsequently swept out to sea (though likely suffered from blunt force trauma and/or drowning in the early stages).
Is that actually true, are there any examples of that?I don’t doubt science can easily explain it, but it’s funny how in some locations a new eruption occurs without warning where there had been no more signs of being a volcanic-prone area than central London
Well, perhaps every volcanically active or recently active area does have similar characteristics, but I am not aware of any others. All of the Canary Islands are of volcanic origin, and several of them have actual extinct volcano calderas peppering their geography, but I am not aware of anywhere in Tenerife or La Palma where you can use the heat from under your feet to cook (see El Diablo ) or pour a jug of water into a pipe going down just a few metres to immediately see an explosive jet of steam shoot back up, as seen in Lanzarote’s Timanfaya National Park to this day.Is that actually true, are there any examples of that?
This isnt a subject I know very much about but all the examples I do know are from areas that are known for volcanic activity. How 'peaceful' a volcano may have been considered to be before it came alive may vary a lot, the amount of warning of increased activity may vary a lot, but have there really been any eruptions in areas where no volcanic activity was suspected in this period of history at all? From what I read the UK hasnt had an active volcano for over 50 million years, so if we did have an eruption then that would certainly count, but are there actually any examples at all of such a thing happening in the modern era?
I'm ignorant about the locations in question, I will try to learn more about this interesting subject!Well, perhaps every volcanically active or recently active area does have similar characteristics, but I am not aware of any others. All of the Canary Islands are of volcanic origin, and several of them have actual extinct volcano calderas peppering their geography, but I am not aware of anywhere in Tenerife or La Palma where you can use the heat from under your feet to cook (see El Diablo ) or pour a jug of water into a pipe going down just a few metres to immediately see an explosive jet of steam shoot back up, as seen in Lanzarote’s Timanfaya National Park to this day.
Yet La Palma experienced a massive two-month eruption last year. I guess it’s as simple an answer as sitting on top of different and unconnected magma chambers with different pressure characteristics. But even so I still find it curious you have one island where for the last two hundred years since the last eruption the chamber underneath has remained active enough to cook your arm in seconds if you were to stick it down a rock fissure at certain places but has not had even the slightest hint of a new eruption, while a nearby island that has been completely dormant suddenly spills out millions of tons of lava without warning.
Activity Summary: Kīlauea volcano is not erupting. An increase in seismicity in the south caldera region started this morning and has remained at high levels since 3 a.m. HST. Kīlauea’s summit remains pressurized; in recent months unrest has escalated quickly, and an eruption could occur in the future with little warning.
Summit Observations: Seismicity began to increase just before midnight. Since 3 a.m. HST, 25-30 locatable earthquakes have occurred per hour at depths of 1.5–3 km (1–2 mi) below the surface. Earthquake clusters have migrated between the area just south of Halema’uma’u and the region southwest of the outer caldera boundary. The most intense activity occurred between 6 and 8 a.m., when earthquakes were clustering just south of Halemaʻumaʻu. There have been over 180 locatable earthquakes in this region in the past 6 hours, with magnitudes ranging from a maximum of 3.4 to less than 1. Several of these earthquakes were large enough to be felt by HVO staff in the field, who also reported rockfalls on the south side of Halemaʻumaʻu.
Models based on GPS data that were reviewed at a meeting this morning (February 1) with scientists from the Icelandic Meteorological Office and the University of Iceland show that approximately 6.5 million cubic meters have now flowed into the magma chamber at Svartsengi. Based on this estimate, it is likely that the magma volume will reach a similar volume as before the January 14 eruption in the next two weeks and even days. This means that the probability of magma flow and eruption has increased.
It is not certain that the notice will be as long as in the last eruption (January 14), but then there was about five hours' notice from the time the earthquake started until the eruption started just south of Hagafell. The warning for the volcanic eruption between Stóra-Scógfell and Sundhnúk on December 18 last was about 90 minutes, but that eruption occurred approximately in the middle of the magma tunnel. In case of repeated magma flows, it is likely that the path for the magma will be easier and this will be accompanied by less seismic activity. However, magma flows are always accompanied by increased micro-seismic activity, and it is most likely that there will be a warning for at least one hour on the eve of a volcanic eruption, which will most likely find its way to the magma tunnel that formed last November 10.