Swarm – Page 78 – Iceland geology

January 3, 2016January 3, 2016

Minor earthquake swarm on Reykjanes ridge and TFZ (Tjörnes Fracture Zone)

The new year (2016) stars with two minor earthquake swarms in Iceland. Both earthquake swarms are small in both earthquake magnitude and number of earthquakes.

Reykjanes Ridge earthquake swarm

The earthquake swarm on the Reykjanes ridge started at 09:08 UTC and lasted until 11:24 UTC. The earthquake swarm has stopped for now, I don’t think it’s over at the moment. It’s difficult to know for sure if an earthquake swarm is over or not in this area, since earthquake swarms are complex and a minor earthquake swarm might start a bigger one few hours later.

The earthquake swarm on the Reykjanes ridge. Copyright of this image belongs to Iceland Met Office.

This earthquake swarm was small in magnitude and the largest earthquake had the magnitude of 2,1. The earthquake swarm is taking place in a volcano that last erupted in 1926 according to Global Volcanism Program. I however don’t think it is connected to any volcano related activity, this appears to be more like a rift earthquake activity.

Tjörnes Fracture Zone (TFZ)

A second earthquake swarm today took place in TFZ. This earthquake swarm was small in magnitude and largest earthquake had the magnitude of 1,9. This earthquake swarm is also rather deep, with deepest earthquake having the depth of 21,9 km (if it was properly located). This might suggest that magma was at work here. This earthquake swarm took place in a volcano that last erupted in the year 1868 (they think) (GVP information). There are two volcanoes in this area and it’s not fully clear what volcano erupted in the year 1868.

The earthquake swarm in TFZ. Copyright of this image belongs to Iceland Met Office.

This earthquake swarm is continuing and has not yet stopped. It remains a question if it is going to grow or start activity in nearby fault, since sometimes activity in one fault on TFZ can trigger earthquake activity in nearby faults. At the moment that has not happened, but it’s difficult to know for sure at the moment.

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December 26, 2015December 27, 2015

Fresh earthquake activity in Bárðarbunga volcano

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Last night (26-December-2015) two magnitude 3,3 earthquakes took place in Bárðarbunga volcano. This earthquake activity was followed by a change in activity on 2 – 4Hz band, I’m not sure why that is, it might signal a inflow of magma at depth into shallow parts of the crust. This is however only guess on my part, this change in signal and it’s origin.

The change in the SIL station can be seen between 25 and 26-December-2015 on the blue line. Copyright of this image belongs to Iceland Met Office.

It is my view that the risk of eruption in Bárðarbunga volcano is increasing fast and Bárðarbunga volcano might erupt without warning at any time. Iceland Met Office holds a different view and that is there is no major risk of eruption in Bárðarbunga volcano at the moment, even if magma continues to flow into Bárðarbunga volcano.

The earthquake activity in Bárðarbunga volcano. Copyright of this image belongs to Iceland Met Office.

The magnitude 3,3 earthquake in north-east part of Bárðarbunga volcano caldera had the depth of 0,1 km. The magnitude 3,3 earthquake in south-east part of the caldera had the depth of 2,5 km. At 08:20 UTC this morning a magnitude 1,0 took place in Bárðarbunga volcano, that earthquake had the dept of 20,3 km and that suggest the magma inflow might be more than current ideas and models suggest (this earthquake is on the edge of the volcano, not far from Tungnafellsjökull volcano). I don’t know what is going to happen next in Bárðarbunga volcano. Since nobody knows for sure what is going to happen next in Bárðarbunga volcano.

Update 1

The earthquake activity in Bárðarbunga volcano has now created a half-circle of earthquakes in the caldera. Over the past 24 hours there has been slight increase in activity in Bárðarbunga volcano after the magnitude 3,3 earthquakes. There has also been some odd harmonic tremor spikes around Bárðarbunga volcano, the problem is that at the moment there is bad weather taking place at this location in Vatnajökull glacier area. So this might just be wind. I have to wait until the weather gets better in order to see if anything changes.

The earthquake activity in Bárðarbunga volcano at 27-December-2015. Copyright of this image belongs to Iceland Met Office.

I don’t know if any more activity is going to take place. This might die down, it is difficult to be sure about what happens next.

Article updated on 27-December-2015 at 17:56 UTC.

December 20, 2015December 20, 2015

Earthquake activity in Bárðarbunga volcano

Last night (20-December-2015) a earthquake activity took place in Bárðarbunga volcano. Largest earthquake in this short earthquake swarm had the magnitude of 3,5 and the second largest earthquake had the magnitude of 3,1. This earthquake activity is shallow and above above 10 km depth and it appears to be result of magma activity in north-eastern part of Bárðarbunga volcano caldera. The earthquakes that took place appear to be long period volcano earthquakes (details can be found here, under b-type earthquake).

Earthquake activity in Bárðarbunga volcano. Copyright of this image belongs to Iceland Met Office.

There clearly is something going on in Bárðarbunga volcano, it is already known that inflation is taking place in Bárðarbunga volcano after the eruption in Holuhraun ended in February-2015. Along with increase in dyke intrusions this clearly suggest that magma pressure is increasing inside Bárðarbunga volcano. What worries me is not the risk of large eruption in Bárðarbunga volcano. The risk in my view is at the moment risk of small eruption taking place, if a small eruption takes place under a glacier it is going to mean glacier flood. Size depends on the eruption size, duration and other factors. Currently there are no signs of imminent eruption, but that might change without warning. The north-eastern part of the Bárðarbunga volcano caldera is in my view weakened structure due to all the earthquake activity for the past 15 (about) months.

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December 16, 2015

Minor dyke intrusion in Bárðarbunga volcano

From 20:10 to 20:14 UTC a minor dyke intrusion took place in Bárðarbunga volcano. This dyke intrusion was small, only lasting those few moments and the largest earthquake had the magnitude of 2,5. Other earthquakes are smaller. Depth was from 15,6 km to 23,2 km. Based on the location, this is clearly a dyke intrusion into Bárðarbunga volcano. It is too small to start an eruption, but suggest that magma processes in Bárðarbunga volcano are starting to increase again.

The dyke intrusion in Bárðarbunga volcano. Copyright of this image belongs to Iceland Met Office.

There is also a change in the SIL station Vonarskarð. What is creating remains unknown. This might be a change in hydrothermal systems under the glacier, but is impossible to know for sure at this point in time. Copyright of this image belongs to Iceland Met Office.

I don’t know if any more earthquake activity is going to take place in Bárðarbunga volcano. Since it is impossible to know what magma does next inside a volcano. At the moment I’m not expecting a eruption in Bárðarbunga volcano.

December 14, 2015December 14, 2015

Update on Prestahnúkur earthquake swarm

The earthquake swarm in Prestahnúkur volcano is ongoing with breaks. The fault that is moving is around 5 to 15 km long at the moment (based on the map). The largest earthquake so far has had the magnitude 3,5 and was felt in nearby towns and farms, the second largest earthquake had the magnitude 3,0. Other earthquakes have been smaller so far.

The earthquake activity today (14-December-2015). Copyright of this image belongs to Iceland Met Office.

I expect this earthquake activity to continue in the next few days to weeks.

The earthquake activity in this area since 1991 (grey circles). New activity are the red circles. Copyright of this image belongs to Iceland Met Office.

The image above is from Week 50 earthquake information website. It can be found here.

Other matters

I’ve been a bit down in the past few days, since I’m living in Iceland and I don’t like it. I don’t belong in Iceland, not sure why that is, it just is. I don’t like the culture (Icelanders are copying U.S culture to some degree, not everything, but many aspects of it), I don’t like the snow and the cold weather. I also don’t like the isolations that follows living in Iceland.

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At the moment I’ve collected money for almost everything. The transfer cost and the first month in rent for the apartment. What is missing is the money for the insurance for the apartment, but I can get a good rent loan for that in Denmark. The insurance amount I have to pay is 9000 DKK (1,206.13€). All that I’m currently waiting for is the Danish Tax (Skat), I’ve been having problem with them for the past few months and that issue has not been resolved yet and that issue is keeping me in Iceland at the moment. Regardless of that, I’ve started preparing my move back to Denmark so that I can move quickly once my last problem has been resolved.

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December 11, 2015December 11, 2015

Earthquake swarm south-west of Langjökull volcano (Prestahnúkur)

Yesterday (10-December-2015) a earthquake swarm started in south-west Langjökull (Prestahnúkur volcano [Wikipedia page here]). Currently the earthquake swarm is ongoing. This is a slow earthquake swarm so far, not creating many earthquake over period of one hour. Largest earthquake so far had the magnitude of 3,2. Other earthquakes have been smaller, but many earthquakes are over 2,5 in magnitude. The largest earthquake was felt in nearby town of Hvanneyri and possibly other farms close to the location where the earthquake swarm is taking place.

The earthquake swarm in south Langjökull volcano (Prestahnúkur). The earthquake swarm is located in one spot. Copyright of this image belongs to Iceland Met Office.

This earthquake activity is appearing on my geophones when it comes to earthquakes over magnitude 1,9. Every 10 to 20 years this area has earthquake swarms that creates earthquakes with magnitude 4,0 and above. Last such earthquake swarm was something over 10 years ago if my memory is correct. At the moment there is nothing suggesting that eruption might happen at this volcano any time soon. Last eruption took place 3500BCE (GVP information).

December 3, 2015

Earthquake swarm in Torfajökull volcano

Today (03-December-2015) a small earthquake swarm took place in Torfajökull volcano. This was a small earthquake swarm and none of the earthquakes did go above magnitude 2,0. Depth suggests that origins of this earthquake swarm can be traced to hydrothermal changes taking place in the volcano.

The earthquake activity in Torfajökull volcano. Copyright of this image belongs to Iceland Met Office.

This type of earthquake activity happens in Torfajökull volcano since magma is at shallow depth in a wide area inside the caldera. Nothing else is expected to happen.

November 18, 2015

Earthquake swarm on the Reykjanes peninsula (Fagradalsfjall mountain)

Yesterday (17-November-2015) and today (18-November-2015) an earthquake swarm started on the Reykjanes peninsula, this earthquake swarm took place in Fagradalsfjall mountain. Total of 80 – 90 earthquakes took place, none of them larger than magnitude 2,1.

The earthquake swarm on the Reykjanes peninsula. Copyright of this image belongs to Iceland Met Office.

This earthquake swarm looks like a fault swarm, rather than anything connected to a volcano. Earthquake activity might continue in this area for next few days, with a risk of earthquakes with magnitude above 3,0 happening.

November 17, 2015November 17, 2015

Fresh earthquake activity in Bárðarbunga volcano

At 12:39 UTC (16-November-2015) a magnitude 3,2 earthquake took place in Bárðarbunga volcano. The depth of this earthquake was only 0,5 km so it was not created by magma movement, rather stress changes in the crust. This earthquake took place in south-east part of the caldera.

The magnitude 3,2 earthquake in Bárðarbunga volcano on 16-November-2015. Copyright of this image belongs to Iceland Met Office.

There seems to be an minor increase in earthquake activity in Bárðarbunga volcano, this was mentioned in news today in Iceland about this earthquake. Iceland Met Office is keeping a watch for any changes that might be taking place in Bárðarbunga volcano and nearby area. Earthquake activity doesn’t appear to be quieting down even if the eruption in Holuhraun is over.

November 15, 2015November 15, 2015

Deep earthquakes close to Trölladyngja (Bárðarbunga volcano)

During the night of 15-November-2015 a swarm of deep earthquakes took place not far from Trölladyngja. The thing about Trölladyngja is directly connected to Bárðarbunga volcano and its eruption cycles. Trölladyngja it self was formed in a eruption in the year 5000 BCE, according to historical overview from Global Volcanism Program. According to some sources, Trölladyngja is a shield volcano, I don’t know if that is exactly correct. Regardless of what type of volcano Trölladyngja is, there is clearly something going on in it. Since this is not the first time I see earthquake swarm at this depth at this location. I doubt that this are stress related changes in the crust due the collapse of Bárðarbunga volcano caldera.

The earthquake activity in Trölladyngja (red dot). Image is from 05:50 UTC. Copyright of this image belongs to Iceland Met Office.

All of the earthquakes taking place were small, the largest had the magnitude of 1,1 and the depth was from 18 – 15 km.

In the early days of the earthquake swarm that started in Bárðarbunga in August-2014 a dyke intrusion pushed into this direction and than it just stopped as it lost the energy, or hit a obstacle that it was unable to break trough.

Image from August-2014. The earthquake activity close to Trölladyngja is clear on this image. Copyright of this image belongs to Iceland Met Office.

I don’t know yet what the chances are for an eruption at this location. More earthquake swarm activity is needed until the magma that is clearly down there breaks up. However the rifting that is taking place in this location might speed things up by unknown factor. This rifting might and possibly is allowing more magma entering this area deep underground without any earthquake activity. It is difficult to know what is going on at this location, so a lot of this is a speculation on what might happen. What actually happens in the end is a whole different thing and only time is going to tell us what happens next.

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