Dyke intrusion in Öræfajökull volcano confirmed

Recent measurement of Öræfajökull volcano have confirmed a dyke intrusion, the dyke intrusion is located in south part of Öræfajökull volcano and that area is showing inflation. At the moment the amount of magma is now estimated at being close to the total of what erupted in 2010 eruption of Eyjafjallajökull volcano. At the moment the dyke is at depth of 2 – 6 km and that explains current hydrothermal activity in Öræfajökull volcano and why it is increasing. How long this is going to go on is not known at the moment. Öræfajökull volcano is a stratovolcano with everything that comes with it (information about this type of voclano can be found here and here).


The earthquake activity in Örfæajökull volcano for the last 48 hours. Copyright of this image belongs to Icelandic Met Office.

Last week total of 160 earthquakes where recorded in Öræfajökull volcano and that is a first time record for Öræfajökull volcano having this many earthquakes since recording of earthquakes started in Öræfajökull volcano (~1995?). Earthquake activity seems to be stable at the moment, when that changes is impossible to know at the moment.

Web cameras

There are now two web cameras. The websites are based on non-dynamic folder settings so this links are going to expire rather quickly.

Fagurhólsmýri web camera (only valid for now)
Web camera bridge (only valid for now)

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Cauldron in Öræfajökull volcano continues to get deeper and wider

Latest news of the cauldron that has formed in Öræfajökull volcano is not good. According to the news on mbl.is the cauldron got larger by 20 meters over a 9 day time period. Current shape of the cauldron now is close to the one of water droplet (according to the news). The hydrothermal activity is expanding to the south at the moment.


Current earthquake activity in Öræfajökull volcano. Copyright of this image belongs to Icelandic Met Office.

Earthquake activity in Öræfajökull volcano is constant, sometimes bad weather is preventing detection of earthquakes. There has been a small increase in magnitude of earthquakes being detected at the moment that change is not large as most earthquakes are below magnitude 1,0.

Icelandic News (in English)

Öræfajökull caldera has deepened considerably (mbl.is)

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Continued earthquake activity in Öræfajökull volcano

Earthquake activity continues in Öræfajökull volcano. There is a small drop in earthquake activity every few hours just before it increases again. This seems to be normal for earthquake like Öræfajökull volcano. The magma in Öræfajökull volcano is expected to be rhyolitic in nature. That explains the nature of the earthquakes swarms that are now taking place.


The earthquake activity in Öræfajökull volcano for the last 48 hours. Copyright of this image belongs to Icelandic Met Office.

Largest earthquake in last 48 hours had the magnitude of 1,7. At the moment larger earthquakes have not yet happened in last few weeks (since the magnitude 3,5 earthquake took place). The earthquakes at the outline and some distance from Öræfajökull volcano seems to be fault lines that move as Öræfajökull volcano continues to inflate. There is some risk of earthquakes at those locations, it is my view that risk is mostly minimal for now at least. I don’t know how the development has been for the cauldron in Öræfajökull volcano caldera since I haven’t seen any news about the development of that area.

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Slow increase in earthquake activity in Öræfajökull volcano

There seems to be a slow increase in earthquake activity in Öræfajökull volcano. For the last 48 hours the number seems to be rising. This is how it looks on this graph from Icelandic Met Office.


Earthquake activity in Öræfajökull volcano from 2005 – today. Copyright of this image belongs to Icelandic Met Office.

This increase in earthquake activity suggest that more magma is pushing up the volcano at faster rate. The main idea now is that the magma that is pushing up Öræfajökull volcano is rhyolite in nature and that seems to be confirmed to an extent by the earthquake activity as it now appearing.


Last 48 hours of earthquake activity in Öræfajökull volcano. The volcano is located in south part of Vatnajökull glacier. Copyright of this image belongs to Icelandic Met Office.

How this develops is a big question due to lack of accurate historical accounts. What is known about the eruption in 1362 was written down up to two centuries later and when that happens lack of accuracy is passed into the written record. The written record for the eruption in 1727 – 1728 is slightly better but is far from being accurate.

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Magma movement in Askja volcano (Dyngjufjöll)

For the past few days there has been a earthquake activity in Askja volcano. All of the earthquakes so far have been small in magnitude and only few have reached magnitude above 1,0. This earthquake activity is due to magma movements and its the first time I have seen it reported at this shallow depth (above 10 km depth).


Earthquake activity in Askja volcano. North of Vatnajökull glacier. There is also activity in Herðubreið to the east, but that’s an unrelated activity and is due to tectonic forces in the area. Copyright of this image belongs to Icelandic Met Office.

There are no clear signs that an eruption is about to happen in Askja volcano or in Dyngjufjöll as this area is also called. If an eruption starts in this area outside of any major water area its only going to erupt lava with minimal risk. Explosive eruption due to water is also a possibility but those are impossible to predict.

Two magnitude 3,9 earthquakes in Bárðarbunga volcano

Today (21-November-2017) at 13:53 and 13:55 UTC two magnitude 3,9 earthquakes happened in Bárðarbunga volcano. This earthquake activity was in the regular area in the north-east part of the Báðarbunga volcano caldera. It remains to be seen if there is any change in conductivity in Jökulsá á Fjöllum following this earthquake swarm.


Earthquake activity in Bárðarbunga volcano today (green stars, red dots). Öræfajökull volcano is quiet today (maybe due to extremely bad weather in this part of Iceland at the moment). Copyright of this image belongs to Icelandic Met Office.

The aftershocks form a interesting line that goes east to west in the caldera. I’ve not seen that form before and it’s interesting to see it. I don’t know yet if it means anything besides a possible fault in the volcano. It takes the glacier water 9 hours to reach the monitoring station at Jökulsá á Fjöllum, Grímsstaðir from the one at Upptyppingar. I don’t know how long it takes the water to reach Upptyppingar from the glacier, it is at least several hours.

Please note that with current high activity I’m getting a bit stressed out with the workload when a lot of things are happening in short period of time.

Current list of unrest volcanoes is this.

Bárðarbunga (continued in September 2015 after the August 2014 – February 2015 eruption)
Öræfajökull
Katla
Askja (deep magma activity, not a major concern at the moment)

Other volcanoes are not a concern until they erupt without warning.

Update on Bárðarbunga volcano and high conductivity in Jökulsá á Fjöllum glacier river

Conductivity remains rather high in Jökulsá á Fjöllum as it has been doing since before 14th of November. The source remains at Bárðarbunga volcano. The conductivity has slowly been getting lower since it peaked before 14th of November (I’m not sure when the peak was). Yesterday (18-November) I did notice the news a little discussion about Bárðarbunga volcano. It was stated that at least one cauldron in the glacier above Bárðarbunga volcano is so hot that is makes a steam trough the glacier. I have also not hear any other details about the reason why conductivity remains rather high in Jökuls á Fjöllum glacier river from the observations yesterday.

The steaming hydrothermal systems means there is a considerable energy in Bárðarbunga volcano system at the moment. This also invites the risk that next eruption cycle in Bárðarbunga volcano is going to large. This also increases the risk of small eruptions that are also hard to detect and might not break the glacier surface, unless they happen close to one of the new hydrothermal areas.


Earthquake activity in Bárðarbunga volcano in the last 48 hours. Copyright of this image belongs to Icelandic Met Office.

When next eruption cycle starts in Bárðarbunga volcano is impossible to know.

Uncertainly level declared for Öræfajökull volcano, aviation code moved to yellow alert

Yesterday the Department of Civil Protection and Emergency Management declared uncertainty level for Öræfajökull volcano. Aviation colour code was also moved up to yellow alert level (can be viewed here).

Current status is that a ice cauldron has formed in the centre of the Öræfajökull volcano caldera. It is about 1 km wide and around 21 to 25 meters deep according to early measurements. This is the first time in documented history that such ice cauldrons has formed in Öræfajökull volcano. It is now believed that the ice cauldron has been emptying it self all week resulting in smell of sulphur in Kvíá glacier river. The glacier river can be viewed here on Google Maps Street View. Currently there is not a lot of earthquake activity happening in Öræfajökull volcano. This is to be expected (I guess). It is also worth noting that Öræfajökull volcano did do in few months what took Eyjafjallajökull volcano 16 years to do until an eruption happened.

There is not a lot of details on earlier eruptions from Öræfajökull volcano. Earliest eruption to our in time took place between 1727 and until 1728 (289 years). Before that an eruption took place in 1362 (655 years) and lasted for five months. Currently I don’t have a lot of information about the current status. This is due to lack of measurements as it was not expected that Öræfajökull volcano would do this even if earthquake activity was happening in the volcano. It was only from October (it seems) that it was figured out that something was going on in Öræfajökull volcano.


No earthquake activity in Öræfajökull volcano during the past 48 hours (blue dot in the south part of the image). Copyright of this image belongs to Icelandic Met Office.

Images of the new ice cauldron can be found here on Icelandic Met Office website.

I’ll post new information in this article as needed. If anything major happens I’ll write a new article.

Article updated at 16:26 UTC. Added information that I forgot.

High conductivity in Jökulsá á Fjöllum glacier river is from Bárðarbunga volcano

It seems that the close to 10 days high conductivity in Jökulsá á Fjöllum glacier river is from Bárðarbunga volcano rather than Kverkfjöll volcano as first thought. New images from the area show this clearly as the river from Kverkfjöll volcano doesn’t show any change and the high conductivity has continued without showing any peak as is normal for glacier floods from the lake in Kverkfjöll volcano.

It remains unclear what is going on. At the moment there aren’t any sign of an eruption having taken place in Bárðarbunga volcano and it remains unclear from where the glacier flood water is coming from since weather has prevented flying over this area in recent days. It is possible that this is just a cauldron the glacier emptying it self, but given how long the high conductivity has been going on it must be a large cauldron. This might also mean bad news for the area where bridges are if a major flood happens without warning due to this change or if an eruption starts suddenly and without much warning.

Icelandic news

Upptök frekar í Bárðarbungu en Gengissigi (Ruv.is, Icelandic)

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Deep earthquakes in Bárðarbunga volcano system and increased conductivity in Jökulsá á fjöllum glacier river

Today (7-November-2017) there has been deep earthquakes taking place in Bárðarbunga volcano system, just south-east of the main volcano. This earthquakes are not strong and only have the magnitude of 16,4 to 18,8 km. This time none of the earthquakes that happened reached magnitude 1,0.


Location of the deep earthquakes is south-east of the main Bárðarbunga volcano. It is marked by three red dots. Copyright of this image belongs to Icelandic Met Office.

It is also in the news that conductivity in Jökulsá á fjöllum glacier river (map of Jökulsá á fjöllum glacier river can be found here) is at all times high and have been increasing for the last two weeks (14 days) and are now the highest ever recorded. It is unclear at the moment why this is happening as no eruption has been detected from Bárðarbunga volcano during this time. The glacier river is also unusually dark for this time of the year and smell of hydrothermal water has also been detected. Current values are 295µ/cm. This is a risky situation if something more happens under the glacier as this area goes close to Road 1 and connected bridges. If a major flood happens those bridges are going to get lost and there is always a risk of more damage happening, but that depends on factors that are impossible to predict.

Icelandic News – Google Translated can be used for raw translation

Aukin rafleiðni í Jökulsá á Fjöllum (Rúv.is)
Aukin rafleiðni í Jökulsá á fjöllum (Vísir.is)
Raf­leiðni í ánni farið hækk­andi (mbl.is)

Update 1

There is a possibility that this might be a glacier flood from Kverkfjöll volcano. That has not been confirmed as of this moment. Glacier flood from Kverkfjöll volcano happen every few years.

Updated Icelandic News

Hlaup hugsanlegt í Jökulsá á Fjöllum (Rúv.is)
Aukin rafleiðni í Jökulsá á Fjöllum bendir til hlaups (Vísir.is)

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Article updated at 22:11 UTC.