Katla volcano geology and features

Here is a short blog post about the geology and the features of Katla volcano. This article is based on science and my knowledge of Katla volcano. It might not be error free and up to date. But I do my best in that regards. But as I cannot afford to buy published or subscribe to web pages that publish science articles about volcanoes in Iceland. I do my best with what I can get for free online (that is often some amount of articles). So my information might be outdated, or might have been replaced by new research that I might not know about. But I use peer-reviewed articles when they are available to me.

Evolution of Katla volcano

Katla volcano is an caldera volcano. It formed in the classic way the caldera forms. The formation of Katla volcano took place around before Holocene, but the data that is available in sediments around Katla volcano only go far as ~8400 years. So it is unknown when Katla volcano formed. Instead of water. Katla caldera has glacier that is from 300 to 740 meters thick where it is thickest. For comparison, Hofsjökull volcano glacier is around 650 meters thick where it is thickest (from what I have read, newer studies might have changed that assessment). The exact age of Katla volcano is currently unknown, but it has been suggested that it is of Pleistocene age (2.6 ma to 11,700 years). The shape and form of Katla volcano during this time period is also unknown today. It is also believed that Eyjafjallajökull volcano is considerable older then Katla volcano. But Eyjafjallajökull volcano is among Iceland oldest volcanoes. Being around 750000 years old according to studies into it.

Katla magma chamber and activity

Katla magma chamber goes trough evolutionary changes every 4000 to 6000 years according to estimates and data gathered by scientists. In the past 12000 years, since last ice age it has gone trough that process twice. But this means current set of magma pluming inside Katla volcano is not going to last for more then few thousands of years at best. I do not know exactly what this changes in Katla volcano pluming mean in terms of eruption. But I find it most likely to be nothing in real terms. It has been noted with study into geological past of Katla volcano that it experiences period of high and low activity. Katla volcano has high and low in it’s eruption activity. Based on data from the past 12.000 years. Currently Katla volcano is having a low period activity. That means fewer eruptions with long quiet time between them. As has been the pattern for the past 1100 years or so. This is according to survey data on activity in Katla volcano for that time period. I do not know if changes in Katla volcano magma chamber influences this low and high period of volcano activity in Katla volcano.

Katla lava

Katla volcano erupts basalt lava normally. On extremely rare occasions Katla volcano erupts magma that is andesite in nature. But that is really rare occurrence in nature. I expect next eruption in Katla volcano to be basalt in nature. But no lava is going to flow due the glacier that is on top of Katla volcano. But that is going to create an ash cloud that is not so different from Grímsfjall volcano ash cloud seen in the May 2011 eruption. As the magma in the two volcanoes are mostly basalt in nature. But that maks for darker but also more large ash particle (less small ash particles). So the ash cloud is not going to create the same problem as Eyjafjallajökull volcano ash cloud did in the year 2010.

Reference articles

Katla volcano, Iceland: magma composition, dynamics and eruption frequency as recorded by Holocene tephra layers (2007)
Bergrún Arna Óladóttir & Olgeir Sigmarsson & Gudrun Larsen & Thor Thordarson

Strong earthquake on Kolbeinsey Island ridge yesterday (06.09.2012)

Yesterday (06.09.2012) there was an earthquake about 200 km off Kolbeinsey Island. It was maybe on the Kolbeinsey Island or on SPAR fault zone in this area. I am not sure what is the actual case here. The earthquake had the magnitude of 4.4 and up to 4.7. Its magnitude has not yet been confirmed (EMSC web page can be found here). I do not know why that it. But this sometimes happen. This earthquake was not felt. But I did record it on my geophone network on two stations.


The location according to IMO. The second green star is an magnitude 3.6 earthquake in Jan Mayen. Copyright of this image belongs to Icelandic Meteorological Office.


The location according to EMSC. Copyright of this image belongs to EMSC.

This earthquake is one the strongest earthquakes that have been taking place in this area for the past few weeks. I do not know what is exactly happening in this area. This might be volcanic activity. But given depth of 2 km there. It is hard to know for sure. As any signs of eruption won’t appear on the surface of the ocean. Given that winter storm season has started in this area. Any sign of eruption are going to lost in the ocean waves. This area of the mid-Atlantic ridge might have more earthquakes in coming days to weeks.

Ongoing earthquake swarm in Breinnisteinsfjöll volcano / SISZ

Since yesterday (02.09.2012) there has been ongoing earthquake swarm in Breinnisteinsfjöll volcano / SISZ (south iceland seismic zone). It is impossible to know how this earthquake swarm is going to proceed. But from what I can tell. It does not seem like it is going to be over any time soon. It is also an possibility that current earthquake swarm is part of an larger stress change in the area. But for now it is too early to know for sure what it means in the long term. Current earthquake activity is ongoing. With almost no breaks or stops. Most earthquakes have the magnitude of 0.1 and up to 2.0. But no larger earthquakes have been detected so far. The first earthquake in this earthquake swarm had the magnitude of ML4.4. Depth of this earthquakes is from 3 to 7 km (in that range).


The earthquake activity in Breinnisteinsfjöll volcano. The earthquakes align them self on an fault line that almost directly north-south direction. Copyright of this image belongs to Icelandic Meteorological Office.

It is impossible to know what is going to happen next in this earthquake swarm. But strong earthquake should not be ruled out for now. This might also activate nearby fault lines if the activity intensifies. As that sometimes happens in Iceland. Whatever happens next in this area. It is worth keeping an eye on the progress of this earthquake swarm.

Icelandic news about this earthquake swarm

Enn skelfur undir Bláfjöllum (mbl.is)
Enn skelfur í Bláfjöllum (Rúv.is)

Harmonic tremor pulse activity maybe in Hamarinn volcano

Today (02.09.2012) a harmonic tremor pulse did start in Hamarinn volcano (best guess) (Bárðarbunga volcano). This harmonic tremor pulses are intermittent and normally last for up to 20 to 30 min., at the time. What is creating them is hard to say. But this might just be hydro-thermal activity taking place in Hamarinn volcano. This might also be magma on the move inside Hamarinn volcano. But nothing is confirmed so far. I do not expect anything to be confirmed any time soon.

The harmonic tremor pluses appear on the end of the traces on this image. They are bit hard to spot for the untrained eye. But they appear as higher then background noise change in the tremor plot image.


The harmonic tremor pulse as it appears on the SIL station at Grímsfjall volcano. This is high resolution image from this IMO web page. Copyright of image belongs to Icelandic Meteorological Office.


The harmonic tremor pulse at Skrokkalda SIL station. Copyright of image belongs to Icelandic Meteorological Office.


The harmonic tremor pulse at jok SIL station. Copyright of image belongs to Icelandic Meteorological Office.


Harmonic tremor pulse at dyn SIL station. Copyright of image belongs to Icelandic Meteorological Office.

It is impossible to know what this means exactly. But so far there are no signs of eruption in the area. This activity is less then activity in July 2011 that was created by an minor eruption in Hamarinn volcano. Stronger harmonic tremor pluses appear on SIL station at longer distance. But for now (when active) most of the activity only appears on SIL stations closest to the Vatnajökull glacier. I am going to continue to monitor the current situation. I will update or make a new blog post about what is going on if anything happens.

Magnitude 3.2 earthquake on the Reykjanes peninsula

Today (01.09.2012) at 16:33 UTC there was an earthquake with the magnitude of ML3.2. The depth was 7.6 km. Following this earthquake there was an swarm of smaller earthquakes following the first earthquake. None of those have been above magnitude 2.0. The earthquake took place in the Reykjanes volcano most likely. But it appears tectonic in nature. Rather then volcanic.


The magnitude ML3.2 earthquake on the Reykjanes peninsula. Copyright of this image belongs to Icelandic Meteorological Office.

It is hard to know for sure if this activity is going to continue. But since this earthquakes. Activity in this area has stopped. But it might resume at later time.

Icelandic news about this earthquake

Jarðskjálfti á Reykjanesskaga (Rúv.is)
3,2 stiga skjálfti við Grindavík (mbl.is)

Earthquake swarm on Kolbeinsey Ridge yesterday (30.08.2012)

Yesterday (30.08.2012) there was an earthquake swarm on Kolbeinsey Ridge. But earthquakes have been taking place there for several weeks already. This earthquake activity seems to be growing in number of earthquakes swarms taking place. In the year 1999 there might have been an dike intrusion or submarine eruption south of Spar Fracture Zone (more details here). Last earthquake swarm that was noticed by the SIL network was exacly two months ago (30.06.2012). My coverage of that can be found here. But it was not in the same place. But that earthquake swarm was south of Kolbeinsey Island, not north of it as was the case yesterday.


The earthquake area in question are the yellow dots north of Iceland on this map from IMO. Copyright of this image belongs to Icelandic Meteorological Office.

What happens next in this area in terms of earthquake activity, or possible volcano activity is hard to impossible to know. As it is really hard to monitor volcanoes and rift zones that are under 2 km deep ocean and good distance from the coast line. However if there is any major earthquake activity in this area. It is going to appear clearly on my geophone network and IMO SIL network in Iceland.

Glacier flood confirmed from western Skaftárkatli cauldron

Today (30.08.2012) an glacier flood was confirmed from the western Skaftárkatli cauldron. This glacier flood is small as expected. But it did take several days longer to appear from Vatnajökull glacier then expected. Some hydro-thermal activity in Hamarinn volcano (Bárðarbunga volcano) seems to be currently taking place at the moment. But some harmonic tremor spikes have been taking place in the past two hours.


Harmonic tremor pulse can be seen at the end of this tremor plot from IMO. It only lasted for about 30 to 60 min. Copyright of this image belongs to Icelandic Meteorological Office.


Harmonic tremor pulse can be seen at the end of this tremor plot from IMO. It only lasted for about 30 to 60 min. Copyright of this image belongs to Icelandic Meteorological Office.


Harmonic tremor pulse can be seen at the end of this tremor plot from IMO. It only lasted for about 30 to 60 min. Copyright of this image belongs to Icelandic Meteorological Office.

It might be that this harmonic tremor signals are coming from other volcano system then Hamarinn volcano. This type of activity has been seen before in Hamarinn volcano and follows glacier floods from it. Given the activity last year. I cannot rule out volcano activity taking place now in Hamarinn volcano. New episode of harmonic tremor is now starting in Hamarinn volcano. Based on early observations . It seems that current activity is behaving in similar manner as did happen in July 2011 when an minor eruption took place in Hamarinn volcano. If that is the case now remains to be seen. But it should be clear in few hours what is exactly going on in Hamarinn volcano following this glacier flood.

Icelandic news about this glacier flood

Skaftárhlaup kom úr katlinum – myndband (Rúv.is, video)
Hlaupið kom úr vestari katlinum (mbl.is)

Earthquake in Brennisteinsfjöll volcano / SISZ earthquake zone

Today (30.08.2012) at 11:59 UTC there was an earthquake with the magnitude of ML3.8 (4.2Mw) in Brennisteinsfjöll volcano / SISZ. But SISZ overlaps this area to some extend. So large earthquakes do happen in this area of Iceland on regular basis. This earthquake was felt in Reykjavík area, south Iceland and some part of western Iceland.


The earthquake location and the following aftershocks. Copyright of this image belongs to Icelandic Meteorological Office.

In around 30 aftershocks have been detected in the area. More aftershock activity in this area cannot be ruled out. This earthquake did appear clearly on my geophones all over Iceland.


The earthquake at Eyrarbakki geophone station. This geophone is the closest to the earthquake. The most movement in this earthquake was on an N-S and E-W fault according to my geophones. This picture is released under CC Licence. See licence page for more details.


This is the earthquake as it was recorded on Heklubyggð geophone. It is the second closest geophone station to this earthquake. This picture is released under CC Licence. See licence page for more details.


Here is the earthquake as it did appear on Skeiðflöt geophone. This picture is released under CC Licence. See licence page for more details.


Here is the earthquake as it did appear on Hvammstangi geophone. This picture is released under CC Licence. See licence page for more details.

It is impossible to know for sure what this earthquake activity means. But earthquake activity in this area of Brennisteinsfjöll volcano did stop around 15:49 UTC. No aftershocks did go above 2.0 in magnitude. More earthquakes in this area should not be ruled out in the next few days to weeks.

Icelandic News about this earthquake

Alltaf von á eftirskjálftum (Rúv.is)
Skjálftinn á enda stórs misgengis (Rúv.is)
Verra ef safnið hefði skemmst (Rúv.is)
Skjálftinn hápunktur – ekki fyrirboði (Rúv.is)
Jörð skalf í dag (Rúv.is. Afternoon radio show about this earthquake in Icelandic)
Jarðskjálftasvæðið undir smásjá sérfræðinga (Vísir.is)
Má búast við nokkrum eftirskjálftum (Vísir.is)
Fólk hljóp á dyr í Litlu Kaffistofunni (Vísir.is)
Jarðskjálftinn var 4,6 stig (Vísir.is)
Á þriðja tug eftirskjálfta hefur mælst (mbl.is)
Jarðskjálfti upp á 4,6 stig (mbl.is)
Snarpur jarðskjálfti á höfuðborgarsvæðinu – Stærsti skjálftinn í 3 ár (Pressan.is)
Jarðskjálftafræðingur: Ekki búið að losa um neina spennu að ráði (Pressan.is)

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)

Still no glacier flood in Skaftá glacier river

For reasons that are unknown. No glacier flood has yet taken place in Skaftá glacier river. Even if the western Skaftárketill cauldron in Vatnajökull glacier has emptied. It is now expected that Hamarinn eastern cauldron is going to empty it self soon. But when that might happen is impossible to know for sure.


Ice-quake activity continues in Vatnajökull glacier. But that suggests the water is on the move under the glacier. Copyright of this image belongs to Iceland Meteorological Office.

The glacier flood is expected to be small. But it won’t go unnoticed once started. As the glacier river get’s darker and conductivity in the water increases greatly during the flood. I am going to try and keep an eye out for more information on this glacier flood.

Icelandic News about this

Ekkert hlaup hafið (Rúv.is)