Category: Ash cloud

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Eruption update at 21:29 UTC

This information is going to go outdated quickly.

This is the current information about the eruption in Bárðarbunga volcano.

Please note: Since I cannot go to the area that is erupting my self (it is closed and I also live in Denmark at the moment). I have to relay on what is being told in the news and released by Icelandic Met Office along with other data. This means that I spend most of the day collecting data and working out what is going on (my view in most cases). This means that in most cases I write post late in the day when daily observation is done.

Current status of the eruption in Bárðarbunga volcano

  • New fissure did open around 2 – 3 km south of the eruption fissure that started erupting 31-August-2014.
  • Comments on this website did notice the eruption around 04:00 UTC on 05-September-2014. At the same time there was an minor increase in harmonic tremor on SIL stations close to the eruption.
  • The new eruption fissure is around 1 – 2 km long. It might get longer as time passes.
  • The new eruption was first reported by the press around 06:00 – 08:00 on Rúv.
  • New cauldron has formed some 6 km in Dyngjujökull glacier. The  glacier in the that area is 300 to 350 meters thick. Last report was that this cauldron was getting deeper during the day.
  • Higher conductivity has been reported in Jökulsá á fjöllum glacier river. That is currently continuing on that last check I did on Icelandic Met Office website.
  • Smell of rotten eggs is now coming from Jökulsá á fjöllum. Normally there is no such smell of that glacier river.
  • Inflation in the dyke continues, not on the same speed as before, but it is ongoing.
  • The rift valley appears to continue expand were he is visible.
  • The air around the eruption site is toxic due to release of SO2, CO, CO2, fluorine gases and other dangerous gases.
  • The water vapour cloud goes up to 4,5 km according to latest measurements.
  • The SO2 goes the way of the wind direction at any given time.
  • The lava field has just 1 km to Jökulsá á fjöllum glacier river. Once the lava enters the river it might start to build a dam and the lava is going to explode and steam a lot in the process.
  • Largest earthquake since midnight was magnitude 5,3 that took place at 01:19 UTC. It took place in Bárðarbunga volcano caldera rim. As other large earthquakes since this events started.
  • Largest earthquake in the dyke area took place at 14:31 UTC and had the magnitude of 3,2. It was under the glacier were most earthquake activity is now taking place.
  • Volcano eruption with ash cloud is now expected to take place. When and exactly where it is going to take place is not known at current time. I don’t think it going to have effects on international flight. But the local effects might be big if wind is in the direction of populated areas of Iceland.

GPS inflation

DYNC_3mrap.svd.05.09.2014.at.20.56.utc
GPS measurements of the inflation that is currently taking place in the dyke. More GPS data can be found here. Copyright of this image belongs to University of Iceland.

Magma continues to flow into the dyke. It is at slower rates than before, but it still flowing into the dyke at rates that current eruption is not powerful enough to equal or drop the pressure inside the dyke. This is going to result in more eruptions as we have already started to see. When and where they are going to take place is something that is not known.

The eruption area is closed to the public

Due to risk of dangerous gases and flood the eruption area is closed to the public. Anyone that is found within the closed zone is going to get heavy fine. Going to this area is also extremely risky sine the area that is now eruption is extremely unstable with the risk of new eruption opening up without warning in the fault area and even outside it (if there is a weakness in the crust the magma is going to go that way). Police in Iceland have already spotted and fined two cars that were trying to enter the closed off area. This area of Iceland is also out in the middle of nowhere. The town is up to 10 hours away in a car (due to bad roads). Weather is also extremely unpredictable and can change without warning. So if you are thinking about going on car or foot. Don’t go!

The good news is that it is still allowed to fly over the area. So get one of those tours. I don’t know what they cost, but I know they take place if weather allows.

News bits

Arrested near the Holuhraun eruption (Rúv.is)
See the lava creeping forward at Holuhraun (Rúv.is, video)
The powers at play beneath the surface (Rúv.is, video)

More news in English can be found here (Rúv.is).

Updates for 06-September-2014

  • As noted by many here there is now news report on how much Bárðarbunga volcano has lowered since 16-August-2014. Bárðarbunga volcano has lowered some 15 meters according to latest measurements. This does not reduces the risk of eruption in Bárðarbunga caldera, in fact, this might increase it by a large margin. Such large drop in a mountain has not happened in Iceland since Askja 1875 when that volcano dropped some 300 meters in one of the largest eruption in the 19th century. According to the news on Rúv the caldera crust is in fact floating the magma that is keeping it up. Part of that magma is now erupting just north of Dyngjökull glacier.
  • Magnitude 5,0 earthquake took place in Bárðarbunga volcano at 05:40 UTC. It was in the NE Bárðarbunga in the caldera rim.
  • The risk of large eruption in Bárðarbunga volcano has increased due the current activity and drop of the caldera (as explained above). When such eruption would take place is impossible to know at this time.
  • The lava field is now just 900 meters from Jökulsá á Fjöllum glacier river. It is going to get into contact with the main stream sometimes in the next 24 hour period.
  • The activity in the new eruption fissure has decreased a little over the past 24 hours. It is now only erupting in one or two craters at the moment.
  • There is high risk of new fissures opening in the rift valley without warning. Both outside the glacier and below it. If an eruption takes place under the glacier there is going to be sudden glacier flood that is going to hit without warning.
  • Possible minor eruption might have happened under Dyngjökull glacier in last few days. As there have been cauldron formations in it. One of the cauldron is some 6 km from the glacier edge. The deepest cauldron is 35 meter deep according to radar measurements.
  • A new cauldron was also found some 10 km from the edge of Dyngjujökull glacier. This suggest that minor eruption took place there in past few days.
  • Blue mist has been seen today in east Iceland. It is not clear what is happening, but there are clues that this blue mist is connected to the eruption. Sensors to measure this blue mist have been sent to east Iceland. This blue mist can also be seen on satellites that Icelandic Met Office uses for weather measurements.

News bits for 06-September-2014

Rannsaka bláa móðu á Austurlandi (Rúv.is, picture of the blue mist, Icelandic)
Eldstöðvarnar í Holuhrauni – Myndband (Rúv.is, Icelandic, video)

Updates for 07-September-2014

  • Earthquake with the magnitude of 5,4 took place at 07:07 UTC. This earthquake took place in the caldera rim as other earthquakes in Bárðarbunga volcano.
  • The flow of magma is currently 100 to 200 m³ every second.
  • The new fissure has stopped erupting according to latest news.
  • There is a high risk of new fissure opening up in the erupting area without warning.
  • The lava field has reached Jökulsá á Fjöllum glacier river. This is going to increase conductivity in the river as the lava goes more into the glacier river. There is a lot of steam cloud being created following this. It is not clear when the lava field is going to dam the glacier river.
  • There are now only 2 – 3 craters erupting in the main erupting fissure. The power of the eruption remains the same.
  • Earthquake activity continues south of current eruption. Most of the earthquake activity now is taking place in the glacier, where minor eruptions have been taking place in past few days.
  • There is no sign of this activity is about to end.
  • Bárðarbunga volcano caldera continues to sink. There is a lack of earthquakes in the caldera it self. That suggest the heat below the crust is high enough to make the crust soft and that prevents earthquakes from happening. More on this tomorrow (Monday).

News bits on 07-September-2014

100 – 200 rúmmetrar úr jörðu á sekúndu (Rúv.is, video, Icelandic)
Svona hefur Bárðarbunga sigið (Rúv.is, picture of the lowering of Bárðarbunga caldera, Icelandic)

Article updated at 14:04 UTC on 06-September-2014.
Article updated at 14:11 UTC on 06-September-2014.
Article updated at 18:16 UTC on 06-September-2014.
Article updated at 18:18 UTC on 06-September-2014.
Article updated at 18:29 UTC on 06-September-2014.
Article updated at 19:43 UTC on 06-September-2014.
Article updated at 14:52 UTC on 07-September-2014.

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Rift valley has formed south of the eruption in Holuhraun lava field

This information is going to get outdated quickly. This is current events in Báðarbunga volcano.

  • Rift valley has formed south of the eruption. Part of this rift valley is not under the glacier. Most of this rift valley is under the glacier, were the glacier is thin the glacier has formed a cauldron that is around 1 km wide and several meters deep. There is a risk of eruption in the newly formed rift valley.
  • Harmonic tremor suggest that an glacier flood is under way from Bárðarbunga volcano. What is happening is unclear at the moment. Scientists and press people have been told to evacuate the area due to this risk.
  • More magma is going into the dyke then is erupting from it. This has increased the pressure inside the dyke.
  • Largest earthquake since midnight had the magnitude 5,5.

Updates

  • There has not been any sign of an eruption under the glacier yet. One idea for this increase in harmonic tremor is that ground water got into contact with the magma at 1 to 2 km depth.
  • There is a high risk of eruption taking place under the glacier in the area of Dyngjujökull glacier, that glacier is south of current eruption and can be seen on the Míla web cameras.
  • There is a lot of cracks in the ground south of the eruption, in some places the ground has dropped some meters down.

Updates on 4-September-2014

  • Largest earthquakes since midnight (04-September-2014) had the magnitude of 4,8 and 4,4.
  • The eruption is now creating  120 to 130 meters tall lava fountains at the moment. No other change has been reported.

News in both Icelandic and English

Mikið af sprungum í jörðinni (Rúv.is, Icelandic, Video, Image)
Hraun­breiðan 9,1 fer­kíló­metri (mbl.is, Icelandic, Pictures)

Notice on commens

I have to approve all comments first time around. This is in order to prevent spam from taking place in my comment section. Spam prevention is the common Captcha puzzle and a maths test. Registered users don’t have to type in captcha word puzzle or the maths test.

Article updated at 00:27 UTC on 04-September-2014.
Article updated at 11:58 UTC on 04-September-2014.
Article updated at 14:01 UTC on 04-September-2014.

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Large cauldron has formed in Dyngjujökull glacier (south of current eruption)

According to latest news a large cauldron has formed in Dyngjujökull glacier. The cauldron is about 1 km wide and it is deep (no mention of how deep it is in the news).

Update 1: No eruption has yet started. It is however now expected to start without warning. The cauldron are forming due an rift valley formation in this area.

I will post more information about is when I have more details.

Article updated at 12:40 UTC.
Article updated at 12:42 UTC.

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More volcano ash in the ash cloud from Eyjafjallajökull volcano according to a new study

According to an new study into the Eyjafjallajökull volcano ash cloud. It appears that more volcano ash was up in the air then originally estimated. The estimation now is that the amount of volcano ash was around 100 times more then expected during the eruption. This has serious implications to air travel in the future if there is a repeat of the Eyjafjallajökull volcano eruption scenario. But most of Eyjafjallajökull volcano ash was small and fine volcano ash that did stay long time up in the air.

This is the conclusion in a study that was made by Mark Woodhouse (and more people) and is published in Journal of Geophysical Research. Sadly I do not have access to this study (I am too poor to do so). So I an only repeat what the Rúv News is saying about this study.

News and links

Öskufallið var meira en við héldum (Rúv.is, Icelandic)
Journal of Geophysical Research

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Explosions are still taking place in Grímsvötn crater

While the activity has almost stopped in Grímsfjall volcano, but there are still explosions taking place in Grímsvötn lake where the eruption took place due to magma going up, explosions take place all over the fissure at random times. That makes travelling to this area really dangerous thing to do. Ash fall is still taking place in Grímsfjall volcano when explosions take place. But the ash fall is limited to the local area in Grímsfjall volcano. Because of this, the official word is that the eruption is not yet over. Even if it just an small eruption at the moment. So far there is no data that suggests that new magma is currently flowing into Grímsfjall volcano. This is according to news in Icelandic media.

An new caldera (correct word?) has formed in the glacier close to the eruption site. But that suggests that a lot of heat is below in the glacier and is creating strong melt where this taking place. This is according to news on Rúv. But they don’t say where this glacier melt is taking place. But it can be assumed that this formation is somewhere close to the current eruption site. But when I know more about this location. I am going to update this post when I can.

Harmonic tremors pulses are still being detected from Grímsfjall volcano up to 200 km away from the volcano. Why they are still taking place while there is no eruption taking place is unknown to me. It is important to notice that currently the harmonic tremor is slowly dropping for now. But it might increase again without any warning. For now there is no way to know what this tremor means for Grímsfjall volcano.

Automatic GPS data from Icelandic Met Office tells an interesting story. According to this data (it might not be 100% accurate due to nature of GPS) Grímsfjall volcano has moved close to 320mm to the west, close to 350mm to the north, it has also lowered down about 250mm. This is major movement in Grímfjall volcano. To compare it with something, Eyjafjallajökull volcano only inflated about 60mm before it did erupt. This is many times more deflation that took place in Grímsfjall volcano then in Eyjafjallajökull volcano for example.

Earthquakes are still taking place SE and SSE of Grímsfjall volcano. There is no volcano at this location. So I am assuming that this are tectonic earthquakes taking place due to stress changes in the crust around Grímsfjall volcano. All earthquakes so far have been small but with the depth from 15 and up to 5 km.

Extra: According to new news (while I was writing this blog post). The Civil Emergency Authority in Iceland has lowered the alert level from danger level to alert level. News about that can be read here (Icelandic, mbl.is)

Icelandic News about this. Google Translate in an maze. It might work or maybe not.

Enn sprengivirkni í Grímsvötnum (Rúv.is, Icelandic)
Jarðeðlisfræðingur: Orðum ofaukið að gosinu sé lokið (Vísir.is, Icelandic)

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The eruption in Grímsvötn / Grímsfjall volcano most likely not over

Here is a interesting paradox. While the eruption it self has currently stopped in Grímsfjall volcano. The tremor chart around Grímsfjall volcano is still acting like there is a eruption ongoing. I do not know why this is like this. But because of that I don’t think that geologist that monitor Grímsvötn eruption in Iceland are not ready to call off this eruption at current time. At least that is what the news did say at 12:20 UTC on Rúv.

They are also issuing warning to people not going to close to the volcano. As explosions due happen and they can throw up rocks that weight up to 1 ton. If anyone gets hit by that rock, that person does not have to worry about what happens next. The save distance for viewing the crater is estimated to be 2 km or more.

I have no idea what happens next. But I am guessing that this eruption might resume soon and without an any warning at all.

The tremor plot at 15:00 UTC. Pictures are from Icelandic Met Office.

This pattern of tremor is interesting. I am yet unsure what it means. But my guess is that this eruption is not over. Even if it has just stopped for now. I normally consider eruption over when the tremor has gone back into background noise (wind, ice, ocean etc..). That has not yet happened with Grímsfjall volcano eruption at this moment.

Update 1: Here is an tremor plot that Icelandic Met Office has released. The article where this picture is from Icelandic Met Office can be read here, it is in english.


Click on the picture for full size. I must point out that this picture is big. Copyright of this picture belongs to Icelandic Met Office.

Blog post updated at 20:46 UTC.

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Grímsvöt eruption appears to be over

Given the current tremor plot on Icelandic Met Office and with reports it seems that the eruption in Grímsvötn (Grímsfjall volcano) is about to be over for now. It is impossible to know if the eruption is going to resume soon or not. But at the moment this eruption seems to be over as it looks now. If it remains like that has to be seen however.

This drop in the eruption has been confirmed by Icelandic Met Office tremor plots.

Tremor plots as of 07:00 UTC. This tremor plots are from Icelandic Met Office web site. Copyright of this pictures belongs to Icelandic Met Office.

Early news this morning in Iceland reported that steam was only coming from the main crater of Grímsvötn.

Other interesting development is that an earthquakes have started to appear SSE of Grímsfjall volcano (Grímsvötn). It is unclear why earthquake are happening at this location. But dike intrusion at this location is not impossible.

The reason for flight problems in Europe is because of the volcano ash that was ejected into atmosphere in the first days of the eruption. It is going take few days for that volcano ash to disappear from the air. Until that happens, it is going to create problems for air traffic.

Update 1: Even if the eruption appears to be over the tremor is still high. I do not know why that is. It is a question why that is or if this is just break in the eruption or not. Only time is going to tell what happens next.

Update 2: There was an news report this morning that before 02:00 UTC there was an spike in activity in Grímsvötn that did shoot the ash cloud up to 8 km. But that spike did only last for few moments before it was over. Rúv has released video here (Windows Media Player) of the eruption site.

Updated at 07:37 UTC.
Updated at 07:50 UTC.
Updated at 08:33 UTC. Blog post title updated.
Updated at 11:42 UTC.
Updated at 12:23 UTC.

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Less powerful eruption in Grímsvötn / Grímsfjall volcano

It has been reported in the news that the eruption in Grímsfjall volcano (also known as Grímsvötn) is getting less powerful as the time passes. This is perfectly normal for an eruption in Grímsfjall volcano.

This can also be seen on tremor plots around Grímsfjall volcano. They clearly show the eruption getting less powerful over time. It has also been reported in the news that the material that is being erupted is now estimated to be 100 tons/second at the moment. But just yesterday it was 1000 tons/second and up to 2000 tons/second. The eruption is currently stable, even if it smaller then it was in the first few days. It is also not certain if this eruption is going to turn into lava eruption. As there seems to be enough water to continue ash phase of the eruption for the next few days.

Grímsfjall SIL station. It clearly shows the eruption getting less powerful over time.

Kálfafell SIL station. It shows the same pattern as Grímsfjall SIL station. Copyright of both pictures belongs to Icelandic Met Office.

In the news it has also been suggested that there might be less or no influx of new magma from great depth. But I do not know for sure if that is just speculation or not.

The ash plume has only got up to 3 to 5 km according to news reports. This means that has dropped a good distance in the last 24 hours. But yesterday it did reach up to 5 to 9 km. So ash is not spreading far away as it did earlier in this eruption. What is creating flight disruption in Europe and over Iceland is the volcano ash that was ejected in the first few days of the eruption. It has also been an big problem in Iceland is the volcano ash that is getting air blown on the ground. The ground is dry so the volcano ash moves easily because of that. Update 1: It has also been reported that the ash that did was ejected on the first day of Grímsvötn eruption was like all the ash ejected in the Eyjafjallajökull volcano eruption in the year 2010. They also say that this eruption was about the size of normal Katla eruption in there own estimate. News about this can be found here (Icelandic, picture)

Scientists did go today up to Vatnajökull glacier in an attempt to get close the eruption site. Flight over the Grísmfjall volcano is also taking place in an attempt to see the eruption site and take measurements of the eruption.

Update 2: There has been an minor spike in the tremor plot in the last hour or so. I do not know why that is. But this suggest that the eruption is growing in power again.

Icelandic News about it. Use Google Translate if you want some funny reporting.

Dregur úr gosvirkni (Rúv.is, Icelandic)
Dregið hefur úr eldsgosinu – umtalsvert minni gosefnaframleiðsla (Vísir.is, Icelandic)
Dregur úr gjóskuframleiðslu (mbl.is, Icelandic)

Please note that information here might get outdated really fast and with no warning at all!

Post updated at 17:57 UTC.

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General overview of Grímsvötn eruption on 23. May 2011 at 20:33 UTC

This is a general overview of Grímsvötn eruption on 23. May 2011 at 20:33 UTC.

Ash cloud: The ash cloud is still going strong. It is however a bit lower then in first few days. Measurements of the ash plume now says that it is between 5 to 9 km. Because of that it does not appear on the radar at IMO. The ash cloud has now been detected all over Iceland, except for the most western part of Iceland (Westfjod). In the areas closest to the main ash cloud the visibility is from 1 meter and up to 500 meters when it is at it’s best. Ash fall is expected to last for the next few days, or until the crater does not get any water into it to make the ash. The ash cloud is expected to reach Scotland tonight (Rúv, Icelandic). BBC News about cancelled flights due the ash cloud. Farmers live stock has started to die due to the ash cloud. It is unknown how the wild life is doing while the ash cloud covers part of south Iceland. Current output of the Grímsfjall volcano is about 1000 to 2000 tons of ash pr second. It was around 10,000 tons of ash pr second during the first days of the eruption.

Rúv News, Öskufall næstu daga (Icelandic, Rúv.is)

Eruption: Even if the ash cloud is lower now. It appears that the eruption is still going strong. In the evening news at Rúv it was reported that there was a chance the magma that powers this eruption might be from a great depth (more then 20 km). Tremor graphs that are online show and suggest that the eruption is still at full power. The reason why they are at lower noise level is most likely due to fewer explosion in the eruption, as less water is in the crater. When water no longer goes into the crater it turns into lava eruption. There is also an speculation that new fissures might open up in this eruption where there is more glacier cover (evening news on Rúv). But that would mean flash glacier flood and new ash cloud when the eruption would break the glacier covering it. But so far this has not happened and is nothing but a speculation. It would mean earthquake activity when the magma would break the crust, as happened when the eruption did start on 21. May 2011.

GPS data: According to report from IMO and University of Iceland the deflation now has been 50 cm to northwest and has subsided 25 cm. According to the report this about 60% larger then after the eruptions in the year 1998 and in the year 2004.

Web cameras: Grímsvötn Míla web cam is now up and running. It should be possible to see the eruption when an ash cloud is not in the way. But so far that has been the case.

Please note that information here might get outdated really fast and with no warning at all!

Updated at 20:42 UTC.

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Grímsfjall/Grímsvötn volcano eruption update at 21:54 UTC

This is a minor update to the Grímsfjall volcano / Grímsvötn eruption.

Process of the eruption: The harmonic tremor on the SIL stations around Grímsvötn is increasing again after it did drop a little bit down earlier today. Following this the ash plume has again appeared on radar images from Icelandic Met Office. Currently however the ash plume is just around 10 km high. According to the news, the eruption is made out of basalt. But that is a common eruption type for Grímsvötn. The ash cloud is formed when hot magma gets into contact with ice and water and explodes on contact. This eruption is now expected to many times larger then the eruption in Eyjafjallajökull volcano last year.

Ash cloud: The ash cloud does now covers most of Iceland, except the northern part of west Iceland (for the moment) and east Iceland (for the moment) but that is expected to change in the next 24 to 48 hours. Ash has been reported in most town in Iceland. That includes Reykjavík, Akureyri, Selfoss (heavy ash cloud) and more. According to web cameras there is heavy ash fall close to Hekla volcano from Grímsfjall volcano (web camera pointed towards Hekla is here, Eyjafjallajökull is here). Due the ash cloud all flight to and from Iceland has been grounded until this ash clouds goes away.

Earthquakes: Few earthquakes are recorded. But only two earthquakes have been recorded around Grímsfjall volcano and close to in the past few hours. But that does not mean that they are not happening. But they might simply be lost in the harmonic tremors from the eruption.

Other: Nothing at the moment.

Please note that information here might get outdated really fast and with no warning at all!