Category: Krýsuvík

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Earthquake activity in Hekla, Katla, Krísuvík and Bárðarbunga volcanoes

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Hekla and Katla volcanoes

I am going to write about both this volcanoes here. Since I am going to be using the same image anyway for both volcanoes.

Yesterday (26.04.2013) there was a magnitude 1.1 earthquake in Hekla voclano. This earthquake was in the same area that triggered uncertainty level to be declared just before Easters in March. It was later cancelled when nothing more happened.

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Earthquake in Hekla volcano. Also on this picture earthquake activity in Katla volcano (read more below). Copyright of this picture belongs to Icelandic Meteorological Office.

Katla volcano has been having some earthquake activity in past days. So far it has just been minor earthquakes and nothing more. But it has been taking place where a minor eruption took place in Katla volcano during the summer of 2011. That minor eruption created a minor glacier flood. But it did destroy a bridge and closed down the ring road (road 1) in this part of Iceland.

While this activity is currently nothing to worry about. It is worth keeping a eye on it. Just in case it increases, or if some other changes start to take place in Katla volcano.

Krísuvík volcano

A minor earthquake swarm took place in Krísuvík volcano today (27.04.2013). The largest earthquake had the magnitude of 1.9. The depth of this earthquakes was around 8.6 km. Activity in this area is normal and there does not seem anything strange about it. But Krísuvík volcano has been having periods of inflation and deflation for the past three years. Earthquake activity increases when Krísuvík volcano is in period of inflation. If that is the case now I do not know.

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Earthquake activity in Krísuvík volcano. Copyright of this picture belongs to Icelandic Meteorological Office.

Bárðarbunga volcano

A minor earthquake swarm took place in Bárðarbunga volcano today. Largest earthquake in this swarm had the magnitude of 1.3. Depth range was from 18.8 km and up to 11.1 km. This earthquake swarm is important. Since it appears that this is a dike intrusion in Bárðarbunga volcano. But a minor dike intrusion also took place in this area few weeks ago. That also resulted in a minor earthquake swarm in this same area.

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Earthquake activity in Bárðarbunga volcano. Most likely due to minor dike intrusion into the volcano. Copyright of this picture belongs to Icelandic Meteorological Office.

A minor dike intrusions into a volcano does not mean a eruption is going to take place. In many Icelandic volcanoes (and around the world also) dike intrusions into the volcanoes are common event and in most cases do not result in any eruptions. But it is worth keep a watch out for this type of eruptions. Since it might signal a more active period ahead in Bárðarbunga volcano. But it might also just equally don’t mean anything. There is no way to know for sure.

Other then this activity. It has been rather quiet in Iceland at the moment. No larger earthquakes have been taking place in the past two weeks since activity slowed down in Tjörnes Fracture Zone.

Blog post updated at 22:32 UTC on 27.04.2013.
Blog post updated at 22:53 UTC on 27.04.2013.

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Deflation stops in Krýsuvík volcano

According to Rúv News today. Deflation has stopped in Krýsuvík volcano. But this is the latest chapter in inflation and deflation episodes that have been taking place in Krýsuvík volcano during the past three years. It is unclear what happens next in Krýsuvík volcano. But an new inflation episode should not be ruled out at this point.

Lat inflation episode started earlier this year (2012) and stopped in May. Then an deflation episode started. It stopped sometimes in August 2012. It is impossible to know for sure when an new inflation episode starts in Krýsuvík volcano. But it is my opinion that is going to be soon. But how soon exactly is impossible to know. Inflation episodes in Krýsuvík volcano have been followed by strong earthquakes swarms. So that are the signs of an inflation period having started in Krýsuvík volcano.

Icelandic news about this

Landsigið er hætt í Krýsuvík (Rúv.is)

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Earthquake swarm in progress in Krýsuvík volcano

Today (18.08.2012) at 15:52 UTC an earthquake swarm did start in Krýsuvík volcano. So far this swarm is not big. With the largest earthquake having magnitude 1.8 according to automatic size. It is impossible to know at this point if this earthquake swarm is going to be strong, or has just ended. So far earthquake activity continues with minor earthquakes.


The earthquake swarm in Krýsuvík volcano. Copyright of this image belongs to Icelandic Meteorological Office.

If the earthquake activity picks up. I am going to do my best to update this blog. But I am on limited 3G internet connection. So it might be a while until update takes place.

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Fish dying in Kleifarvatn lake due to increasing toxic and hydro-thermal activity

According to Icelandic news today. Fish has been dying in Kleifarvatn lake. But Kleifarvatn lake is inside Krísuvík volcano system. The exact reason why the fish is dying is not known at this point. But report suggests that large amount of fish has been seen dead already. I do not know how much fish there is in Kleifarvatn lake.

This suggests that hydro-thermal and hot spring activity in increasing in the lake. This also suggest that increased toxic levels (for the fish) are now changing in the lake. What toxins are at work here I do not know. But it can be assumed that it is what comes with magma.

For the past three to four years. Krísuvík volcano has been inflating and deflating at regular time intervals. What this means in unclear at present time. But this is signs of increased activity in the volcano anyway. Hydro-thermal and hot spring activity has also been increasing during this period. This has also been followed by increased earthquake activity in Krísuvík volcano when inflation takes place. What happens next is impossible to know for sure. But it is clear that Krísuvík volcano is still far away from erupting any time soon.

Icelandic news about this

Fiskar í Kleifarvatni sagðir í andarslitrum (Vísir.is)
Fiskar i Kleifarvatni sagðir drepast í stórum stíl (Vísir.is)

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Minor earthquake swarms in Iceland

It has been quiet in Iceland during the past few weeks. Besides activity in Katla volcano and Kolbeinsey ridge. Nothing of interest has been going on in Iceland. Here is however the overview of activity in Iceland during the past few hours.

Kolbeinsey Ridge

Some minor earthquake activity has been taking place in Kolbeinsey Ridge during the past few hours. This earthquake swarm is small in nature, with largest earthquakes reaching the magnitude 2.4. Otherwise it remains quiet in this area.


Earthquake activity in Kolbeinsey Ridge. Just north of Grímsey Island. Copyright of this image belongs to Iceland Meteorological Office.

Kolbeinsey ridge has seen some activity during past few weeks. But it might just be normal tectonic earthquakes taking place. So far nothing suggest any volcanism nature of this earthquake activity.

Krýsuvík volcano

During the past few hours. Krýsuvík volcano did see some earthquake activity. This activity is most likely to be tectonic in nature. As Reykjanes peninsula has frequent earthquake swarm that are tectonic in nature.


Earthquake swarm on Reykjanes. It is located within Krýsuvík volcano. This was small earthquake swarm. Copyright of this image belongs to Iceland Meteorological Office.

It remains rather quiet on Reykjanes besides this minor earthquake swarm today.

Katla volcano

After rather interesting activity during the past few weeks. It seems that Katla volcano is slowing down in earthquake activity. For now at least. But it is impossible to know for sure if current quiet sense is going to continue in Katla volcano.


Earthquake activity in Katla volcano during past few days. The activity is mostly concentrated into Katla volcano caldera. Copyright of this image belongs to Iceland Meteorological Office.

Besides this top of the activity. All is quiet in Iceland. Both in volcanoes and earthquakes. That might however change at any time without warning. It happens often in Iceland. I also want to remind people of my geophone web page. Where earthquakes can sometimes be seen soon after they have taken place.

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Krísuvík volcano inflates and deflates regularly

It seems that Krísuvík volcano is inflating and deflating on regular basic. I do not know how regular this change is. But it has been noticed by Icelandic scientists how are bit puzzled by this behavior. Last inflation episode did last until end of the year 2011. Since then deflation did start again and is currently ongoing. It is uncertain if what this means. At the moment it is too early to know for sure if this means if that Krísuvík volcano is getting ready for an eruption. But if there was an eruption in Krísuvík volcano, it would be Hawaiian eruption so no volcano ash. Volcano ash eruption would only take place if an eruption started in Kleifarvatn lake. But the effects of that would be limited to local area (Reykjavík and other nearby towns). It would not create any global problems, as many would want to believe.

Inflation and deflation period have been the years 2009, from January to September. In May 2010 inflation did start again, that inflation period lasted until end of the year 2011. Since then deflation has been taking place. Today there is continues GPS monitoring in Krísuvík volcano. But it is unknown if this type of behavior has taken place before in Krísuvík volcano. But for now Krísuvík volcano is being monitored both with GPS and the SIL network. What happens next anyone guess.

Icelandic news about this.

Land rís og sígur í Krýsuvík (Rúv.is)

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Minor earthquake activity in Iceland

During the past few weeks it has been quiet in Iceland. Really quiet, with almost nothing going on. It is still like that to some extent. So this is just a short overview of the small activity that has been taking place in Iceland during the past 48 hours or so.


The earthquake activity in Iceland during the past 48 hours. Copyright of this image belongs to Iceland Met Office.

The most activity in the last 48 hours have been on the Reykjanes and on TFZ. But there was an small earthquake swarm in each area. With earthquakes that did not get over ML2.5 in size so far. Two earthquakes where in Askja volcano. One in Grímsfjall volcano fissure system (maybe in Þórðarhyrna volcano).


Earthquake west of Hekla volcano, in the SISZ. This picture is released under Creative Common Licencee. See the licence page for more detail.

Katla volcano

During this winter. Katla volcano has been quiet. This is somewhat normal, as more snow means more ice-mass on top of the volcano. But now that has started to melt a little and that means less ice-mass on top of the volcano. That could mean more activity in Katla volcnao during the next few weeks. So far however the activity remains small and there are no special earthquakes to report.


Earthquake activity in Katla volcano, on this picture earthquake activity west of Hekla volcano can also been seen here. Copyright of this image belongs to Iceland Met Office.

The earthquakes west of Hekla volcano belong to the SISZ fault area. Not Hekla volcano it self. What is also interesting is the earthquake activity in south part of Katla volcano. In area outside of the glacier. This are small earthquakes, that do not appear on my geophone. Even if they are close to it. I am unsure what this means for the future. But it is worth keeping an eye on it.

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Analysis of the Helgafell mountain earthquake on Reykjanes

Icelandic Met Office has posted an interesting analysis of the last weeks earthquake on the Reykjanes. But this earthquakes where connected to Krýsuvík volcano activity. By relocating the earthquakes, it is possible for Iceland Met Office to see better how long and how deep the fault that created this earthquakes is. In this case, it was around 2 km long and the movement was east-west, like the one found on SISZ.


The re-located earthquakes. The green ones are normal locations, the orange ones are re-located earthquakes. Copyright of this image belongs to Iceland Met Office.

The orange ones are re-located using relative locations. I am not sure how this technique works. But it often gives better image on what is going on with the earthquakes. Both in terms of the fissure making the earthquakes and the depth where they are taking place.

The fissure in question was on N-S axes and is inclined about 70° in west direction. According to IMO, the aftershocks suggest that movement of this fissure was right slip, along with minor drop in it. That means this according to IMO. The west part of the fissure moved to north and down, while the west part of the fissure moved to the south and little bit upwards. According to IMO. This movements happens in SISZ on large fissures there (when they break).

I am currently waiting for more earthquakes in this area. This activity is not over in my opinion any time soon.

Source of data: Week 9 – Iceland Met Office (Icelandic).

Other: I am sorry for lack of updates. There has not been anything special going on and I have been working on confirming getting an apartment in May 2012.

Blog post updated at 09.03.2012 at 17:37 CET. Fixed spelling error.

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More earthquakes should be expected on the Reykjanes

The earthquake swarm on the Reykjanes has slowed down considerable since it did start yesterday. But it is still ongoing in my opinion. Even if there are no earthquakes currently taking place at the moment. There are several reasons for this. The biggest one is that this area seems to be getting more active now then it has been for many decades now. The fissure that is currently moving is connected to Krýsuvík volcano, but this was reported in the news. I do not know every fault line in this area and how they are connected (plus, my volcano map is in an box until I move back to Denmark) together. But I do know that

During the past 2 to 3 years the volcano Krísuvík has been showing more activity. With inflation and deflation episodes that lasts from few days to weeks at the time. Followed by an earthquake swarms both before and after each episode of activity. This activity seems to be increasing, at least that is my opinion on what is happening at the moment.

While this earthquake swarm is still ongoing. It might have long periods of no activity at all. This is common for faults that have not moved in an long time. As seems to be the case in Helgafell mountain and nearby area. But the fault lies close to that mountain or under it (I am not sure). But this started this year with an magnitude ML3.2 earthquake in this area earlier this year.

It is hard to know exactly when next episode of this activity is going to continue. But I am sure that it is going to be soon.

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A ML3.6 earthquake in Krísuvík volcano (automatic size)

At 21:12 UTC on 3. January 2012 an earthquake with the automatic size of ML3.6 did happen in Krísuvík volcano. I do not yet know if this earthquake was felt in the nearby area. But I assuming that it has done so.

This earthquake did appear clearly on my geophones. Both in north and south Iceland. They can be viewed here. I am going to update this blog post as I know more. But this seems to be an start of earthquake swarm in Krísuvík volcano.

Update 1: It has been confirmed that this earthquake was felt in Reykjavík and nearby area. The automatic depth of this earthquake was 14.2 km according to Iceland Met Office.

Update 2: Earthquake swarm has started in Krísuvík volcano. The largest earthquake in this earthquake swarm after the main earthquake is ML1.1 in size. Larger earthquakes however might happen at any time in this earthquake swarm. But that is at least the experience so far.

Update 3: Here are the traces of the earthquake. Sorry. But for the moment there are no high resolution pictures available as my main earthquake computer is offline until I move back to Denmark. See this blog post here for more details on that.


The location of the ML3.6 to ML3.7 earthquake in Krísuvík volcano. Copyright of this picture belongs to Iceland Met Office.


The ML3.6 earthquake as it did appear on Eyrarbakki geophone. This picture is released under Creative Commons Licence. Please see the CC Licence web page for more detail.


The ML3.6 earthquake as it did appear on the Heklubyggð geophone. This picture is released under Creative Commons Licence. Please see the CC Licence web page for more detail.


The ML3.6 earthquake as it did appear on the Hvammstangi geophone. This picture is released under Creative Commons Licence. Please see the CC Licence web page for more detail.

Blog post updated at 21:38 UTC.
Blog post updated at 21:45 UTC.
Blog post updated at 22:15 UTC.