Showing posts with label Iceland. Show all posts
Showing posts with label Iceland. Show all posts

Thursday, 30 May 2024

Town of Grindavik evacuated again as new eruption begins on the Reykjanes Peninsula, Iceland.

Eruptive activity on the Reykjanes Peninsula, Iceland began again on 29 May 2024, according to the Icelandic Met Office, the first such eruption since activity on a fissure which opened in March petered out three weeks ago. The activity is thought to have started when magma flowing from the magma reservoir beneath Svartsengi into the area beneath the Sundhnúkur crater row. At about 4.00 pm on 29 May the magma encountered groundwater penetrating through a fissure from a previous eruption, leading to a phreatic explosion as a large volume of the water was turned into steam instantly. This led to the formation of a new fissure running southwest to northeast (parallel to previous fissures on the peninsula) for about 2.4 km. This fissure has produced lava fountains up to 50 m high, and is extruding lava at a rate of about 1500-2000 m³ per second. The eruption has prompted the evacuation of the town of Grindavik, and the nearby Blue Lagoon Geothermal Spa. The fissure is further from the town than the eruption in January which saw lava entering the streets of the settlement and several buildings destroyed, but is also significantly larger, and is evolving significant amounts of toxic gasses.

A volcanic fssure on the Reykjanes Peninsula, Iceland, which opened on 29 May 2024. Marco Di Marco/AP.

Although dramatic, lava flows are not usually considered particularly dangerous, as their advancing fronts are quite slow and can quickly be outpaced by an able-bodied Human being. The more deadly volcanic events are pyroclastic flows, such as the one which engulphed the Roman town of Pompeii, in which clouds of superheated gas and ash move downhill at high speeds in an avalanche-like motion, and phreatic explosions, caused by bodies of lava encountering bodies of water, which evaporate almost instantly, causing huge explosions.

The size and position of the new fissure on the Reykjanes Peninsula, Iceland. Icelandic Met Office/BBC.

Iceland lies directly upon the Mid-Atlantic Ridge, a chain of (mostly) submerged volcanoes running the length of the Atlantic Ocean along which the ocean is splitting apart, with new material forming at the fringes of the North American and European Plates beneath the sea (or, in Iceland, above it). The Atlantic is spreading at an average rate of 25 mm per year, with new seafloor being produced along the rift volcanically, i.e. by basaltic magma erupting from below. The ridge itself takes the form of a chain of volcanic mountains running the length of the ocean, fed by the upwelling of magma beneath the diverging plates. In places this produces volcanic activity above the waves, in the Azores, on Iceland and on Jan Mayen Island. All of this results in considerable Earth-movement beneath Iceland, where Earthquakes are a frequent event.

The passage of the Mid-Atlantic Ridge beneath Iceland. NOAA National Geophysical Data Center.

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Sunday, 14 January 2024

Lava from new volcanic fissure reaches the town of Grindavik, Iceland.

A flow of lava from a new fissure associated with the Fagradalsfjall Volcano on the Reykjanes Peninsula has reached the town of Grindavik, following a new erruption on Sunday 14 January 2024. The town was evacuated when the fissuere first opened in November 2023, so the lava flows are thought to present no threat to Human life, but at least one property has been destroyed, and it is likely that the lava will keep flowing for some time, doing further damage to the town's infrastructure.

A flow od lava entering the town of Grindavik. Eggert Jóhannesson/Morgunbladid.

Although dramatic, lava flows are not usually considered particularly dangerous, as their advancing fronts are quite slow and can quickly be outpaced by an able-bodied Human being. The more deadly volcanic events are pyroclastic flows, such as the one which engulphed the Roman town of Pompeii, in which clouds of superheated gas and ash move downhill at high speeds in an avalanche-like motion, and phreatic explosions, caused by bodies of lava encountering bodies of water, which evaporate almost instantly, causing huge explosions.

An aerial photograph of the 14 January 2024 eruption, showing its proximity to the town of Grindvik. Iceland Civil Protection/Reuters.

Iceland lies directly upon the Mid-Atlantic Ridge, a chain of (mostly) submerged volcanoes running the length of the Atlantic Ocean along which the ocean is splitting apart, with new material forming at the fringes of the North American and European Plates beneath the sea (or, in Iceland, above it). The Atlantic is spreading at an average rate of 25 mm per year, with new seafloor being produced along the rift volcanically, i.e. by basaltic magma erupting from below. The ridge itself takes the form of a chain of volcanic mountains running the length of the ocean, fed by the upwelling of magma beneath the diverging plates. In places this produces volcanic activity above the waves, in the Azores, on Iceland and on Jan Mayen Island. All of this results in considerable Earth-movement beneath Iceland, where Earthquakes are a frequent event.

The passage of the Mid-Atlantic Ridge beneath Iceland. NOAA National Geophysical Data Center.

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Wednesday, 20 December 2023

Volcanic eruption on the Reykjanes Peninsula, Iceland.

On 11 November 2023 residents of the town of Grindavík on the Reykjanes Peninsula, Iceland, were evacuated from their homes following a major increase in seismic activity beneath the nearby Fagradalsfjall Volcano. The evacuations were triggered by the discovery of a magma tunnel running directly beneath the town at a depth of about 1.5 km. This is about 12 km long, originating near Stóra-Skógfell hill, and running beneath the town and some way out to sea. Seismic activity in the area has remained high in the area in the intervening weeks, although some people had begun to return to their homes. 

Slightly after 10.15 pm on Monday 18 December 2023, a new volcanic fissure opened on the peninsula, spewing vast amounts of lava and prompting a new series of evacuations. The fissure is about 3.5 km in length, and about 3 km from the town of Grindavík. It is currently producing 100-200 m³ of lava per second, although this is not flowing towards the town, and is not thought to present a threat to Human life.

Lava spewing from a new volcanic fissure on the Reykjanes Peninsula, Iceland, which opened on Monday 18 December 2023. BBC.

Although dramatic, lava flows are not usually considered particularly dangerous, as their advancing fronts are quite slow and can quickly be outpaced by an able-bodied Human being. The more deadly volcanic events are pyroclastic flows, such as the one which engulphed the Roman town of Pompeii, in which clouds of superheated gas and ash move downhill at high speeds in an avalanche-like motion, and phreatic explosions, caused by bodies of lava encountering bodies of water, which evaporate almost instantly, causing huge explosions.

People watching a lava flow on the Reykjanes Peninsula, Iceland, this week. Kristin Elisabet Gunnarsdottir/AFP/Getty Images.

Iceland lies directly upon the Mid-Atlantic Ridge, a chain of (mostly) submerged volcanoes running the length of the Atlantic Ocean along which the ocean is splitting apart, with new material forming at the fringes of the North American and European Plates beneath the sea (or, in Iceland, above it). The Atlantic is spreading at an average rate of 25 mm per year, with new seafloor being produced along the rift volcanically, i.e. by basaltic magma erupting from below. The ridge itself takes the form of a chain of volcanic mountains running the length of the ocean, fed by the upwelling of magma beneath the diverging plates. In places this produces volcanic activity above the waves, in the Azores, on Iceland and on Jan Mayen Island. All of this results in considerable Earth-movement beneath Iceland, where Earthquakes are a frequent event.

The passage of the Mid-Atlantic Ridge beneath Iceland. NOAA National Geophysical Data Center.

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Sunday, 12 November 2023

Icelandic town evacuated due to concerns about volcanic eruption.

The town of Grindavík on the Reykjanes Peninsula, Iceland, which has about 3000 permanent residents plus a thriving tourism industry, was evacuated on Saturday 11 November 2023, following a sharp increase in Earthquakes in the area, which geologists fear may be linked to an imminent eruption from the nearby Fagradalsfjall Volcano. Iceland, which is an Earthquake-prone country with numerous active volcanic fields, began to suffer an increase in seismic activity on 25 October, since when it has suffered around 22 000 Earthquakes, with the Reykjanes Peninsula being particularly affected. In the 24 hours before the evacuation was ordered, 1400 Earthquakes were reported beneath Iceland, 880 of them beneath the Reykjanes Peninsula.

A crack in a road in the town of Grindavík on the Reykjanes Peninsula, Iceland, caused by an Earthquake this week. Ragnar Visage/RÚV/Reuters.

The evacuations were triggered by the discovery of a magma tunnel running directly beneath the town at a depth of about 1.5 km. This is about 12 km long, originating near Stóra-Skógfell hill, and running beneath the town and some way out to sea. There appears to be a considerable amount of lava in this tunnel, leading to fears that any eruption would be considerably larger than the Vestmannaeyjar eruption of 1973, in which a 3 km long fissure opened, resulting in the destruction of 400 homes, and an ashfall which covered most of Iceland, reaching 5 m deep in places, although only a single person lost their life. 

The length of the magma tunnel and its position partly under the town of Grindavík.  Kristrún Eyjólfsdóttir/RÚV.

Iceland lies directly upon the Mid-Atlantic Ridge, a chain of (mostly) submerged volcanoes running the length of the Atlantic Ocean along which the ocean is splitting apart, with new material forming at the fringes of the North American and European Plates beneath the sea (or, in Iceland, above it). The Atlantic is spreading at an average rate of 25 mm per year, with new seafloor being produced along the rift volcanically, i.e. by basaltic magma erupting from below. The ridge itself takes the form of a chain of volcanic mountains running the length of the ocean, fed by the upwelling of magma beneath the diverging plates. In places this produces volcanic activity above the waves, in the Azores, on Iceland and on Jan Mayen Island. All of this results in considerable Earth-movement beneath Iceland, where Earthquakes are a frequent event.

The passage of the Mid-Atlantic Ridge beneath Iceland. NOAA National Geophysical Data Center.

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Monday, 9 January 2023

Looking for variations in Human generation times over the past 250 000 years.

Generation time, i.e. the difference in age between parents and their children, is thought to have played a major role in Human history, and it is common to refer to significant events, such as the reaching of new landmasses or exchanging DNA with other Hominids, as having happened a number of generations ago. When such statements are made, it is generally assumed that generation times will have remained constant throughout Human history, and that we can estimate the number of generations to have passed since a particular event by extrapolating from the generation times of modern hunter-gatherer populations. However, there is no particular reason to believe that either assumption is true; population times among modern Human societies are known to vary independently for males and females, and in response to a wide range of social and environmental factors, while generation times vary considerably between different groups of modern hunter-gatherers. Furthermore, generation time can be shown to have evolved since our separation from our nearest Ape relatives, as well as within the Great Apes as a group.

Another method used in previous attempts to estimate the generation time of past Humans has been to use the rate at which DNA mutates between generations, measured against samples of ancient DNA from 40 000-45 000 years ago. This probably gives a more realistic estimate of the number of generations that have passed, and therefore the length of each generation, but is averaged across both genders, and only looks a limited distance into the past.

In a paper published in the journal Science Advances on 6 January 2023, Richard Wang of the Department of Biology and Department of Computer Science at Indiana University Bloomington, Samer Al-Saffar, also of the Department of Computer Science at Indiana University Bloomington, Jeffrey Rogers of the Human Genome Sequencing Center and Department of Molecular and Human Genetics at Baylor College of Medicine, and Matthew Hahn, again of the Department of Biology and Department of Computer Science at Indiana University Bloomington, present the results of an attempt to estimate Human generation times, for both sexes and across several different populations, spanning the past 250 000 years.

As Humans age, they accumulate an increasing number of mutations in their genetic code, and pass this on to their descendants. Wang et al. used data from an Icelandic study, in which the ages of parents at the time of conception were known, to model the six potential types of single nucleotide mutations, establishing that some became significantly more common with age, while others did not, thus providing a clock by which to estimate the age of unknown parents at the time of conception. 

The mutation spectrum changes with human generation time. (A) Data on de novo mutations from 1247 Icelandic trios were used to train a model that predicts the effect of both maternal and paternal age on the mutation spectrum. (B) Data from 25.3 million segregating variants whose date of origin was estimated were used to assess the mutation spectrum at different periods in the past. The mutation spectrum from each time period (bin) was used as input to the model from (A) to estimate the generation interval for males and females. (C) Differences in the frequency of each of the six different mutation types through time, as compared to the most recent time period (smoothed lines from local regression). Wang et al. (2022).

All living Humans are thought to be descended from a single population living about 250 000 years ago. By combining this with their data on age related mutation rates, Wang et al. estimate that the average generation time over this period has been 26.9±3.4 years. Furthermore, they were able to record differences between the sexes in their data, giving an average male generation time of 30.7±4.8 years, and an average female generation time of 23.2±2.0 years. Furthermore, Wang et al. are able to detect changes in the signal over time, suggesting that the average Human generation span was 24.9±3.5 years about 250 generations (or approximately 6700 years) ago, having declined from a peak of 29.8±4.1 years about 1400 generations (or approximately 38 000 years) ago, which would have been just before the Last Glacial Maximum. These estimates are, however, across multiple Human populations.

The study shows a longer generation time for males than females across all timespans, something which tallies with our understanding of modern Human cultures, 99% of which typically see such a longer male generation interval. Wang et al. note that much of the variance in generation intervals seem over time is connected to male generation intervals, while female intervals remain more constant. They suggest that the reason for this is likely biological rather than cultural, with Male humans typically remaining fertile for about 20 years longer than females. This creates the possibility for social structures to create considerably more variation in male generation time than in female generation time. Thus the difference in average generation time is strongly connected to a difference in male generation time in all but the most recent period, during which an overall increase in generation time has been linked to an increase in both male and female generation intervals, and the female generation interval appears to be larger than at any point in the past 250 000 years.

Wang et al. also looked at variations in generation interval between Human populations, considering four major geographical groups, Africans, Europeans, South Asians, and East Asians, although they note that beyond about 2000 generations ago the ancestors of all of these groups were likely to have been living in Africa, while about 10 000 generations ago all of these groups would have been descended from the same ancestors.

It was found that over the past 1000 generations, the average generation time for European and South Asian populations had increased slightly, while that for East Asian and African populations had remained relatively constant. Over the past 40 000 years, Europeans have had an average generation time of 26.1 years, slightly lower than the East Asian average of 27.1 years, but beyond this, the generation time for all non-African populations grows progressively shorter further into the past. Over the past 10 000 generations all non-African populations have shown significantly lower average generation times than African populations, with an average of 20.1±3.9 for East Asians, 20.6±3.8 for Europeans, and 21.0±3.7 for South Asians, compared to 26.9±3.5 for Africans.

This strongly suggests that different time scales should be used to calculate generation length in Africa (roughly 27 years per generation) and outside Africa (20-21 years per generation). Wang et al. note that, since the generation times for non-Africans dating back more than 2000 generations, when they would presumably have been living in Africa, these differences are in fact between different groups living on the same continent, suggesting that considerable variation in the population on that continent (which is considerably genetically more diverse than the rest of the planet) may remain hidden.

Change in generation interval across different Human populations. Generation intervals were estimated in ancestors of four major continental Human populations included in the 1000 Genomes Project; sex-averaged generation intervals are shown here. Confidence intervals for each population were  obtained by bootstrapping. The inset shows results from including polymorphisms that  date back to 78 000 generations ago; note that  age estimates of mutations in the very distant past  have  decreased accuracy. Abbreviations: AFR, Africa; EAS, East  Asia; EUR, Europe; SAS, South Asia. Wang et al. (2023).

Wang et al.'s study improves considerably on our previous understanding of the spontaneity of genetic mutations, and uses this information to make estimates about Human generation times in the past which were previously impossible. Their results are compatible with previous studies which have estimated generation times over the past 40 000 years, but extend the period covered by the estimate back much further, to 250 000 years before the present. While they suspect that the convergence of the Human race back to a single population about 10 000 generations in the past will prevent this model from looking back any further, Wang et al. believe that larger data sets may in the future allow for a much more detailed understanding of generation times within individual populations over the past 100 generations, particularly as parts of this period can be covered by historical birth records.

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Saturday, 27 March 2021

Eruption on Mount Fagradalsfjall, Iceland.

The Icelandic Meteorological Office has reported an eruption on Mount Fagradalsfjall, part of the Krýsuvík-Trölladyngja Volcanic System, on the Reykjanes Peninsula. The eruption started at about 8.45 pm local time on Friday 19 March 2021, with a fissure 500-700 m in length opening up to the southeast of the main volcano, and produced lava fountains up to about 100 m high, with the lava spreading to cover an area of about 1 km² by the next day. The eruption persisted for several days, but decreased in intensity steadily. While spectacular, the eruption was not particularly dangerous, attracting large crowds of onlookers, some of whom took the opportunity to cook sausages on the cooling lava.

 
Crowds of onlookers watch a fissure eruption to the southeast of Mount Fagradalsfjall on the Reykjanes Peninsula, Iceland. AFP/Getty Images.

The Krýsuvík-Trölladyngja Volcanic System comprises a composite fissure swarm about 50 km in length, with no central volcano, but several small shields (i.e. volcanic structures made up largely of overlapping lava deposits that resemble upturned bowls rather than a cone) including Mount Fagradalsfjall. The system has been essentially quiet for about 800 years, with the last known eruption happening in the fourteenth century, and the last major eruption two centuries before that. However, an eruption in the area was expected, as a very large number (over 50 000) of earthquakes had been recorded beneath the system over the past few weeks, something which is often indicative of fresh magma moving into chambers beneath inactive volcanoes.

 
Earthquakes with a Magnitude of 4.0 or greater on the Reykjanes Peninsula over the past 30 days. USGS.

Iceland lies directly upon the Mid-Atlantic Ridge, a chain of (mostly) submerged volcanoes running the length of the Atlantic Ocean along which the ocean is splitting apart, with new material forming at the fringes of the North American and European Plates beneath the sea (or, in Iceland, above it). The Atlantic is spreading at an average rate of 25 mm per year, with new seafloor being produced along the rift volcanically, i.e. by basaltic magma erupting from below. The ridge itself takes the form of a chain of volcanic mountains running the length of the ocean, fed by the upwelling of magma beneath the diverging plates. In places this produces volcanic activity above the waves, in the Azores, on Iceland and on Jan Mayen Island. All of this results in considerable Earth-movement beneath Iceland, where Earthquakes are a frequent event.

 
The passage of the Mid-Atlantic Ridge beneath Iceland. NOAA National Geophysical Data Center.

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