Volcano – Page 99 – Iceland geology

March 17, 2014

More magma in Hekla magma chamber then before 2000 eruption

According to news today on mbl.is there is now more magma in Hekla volcano then before the 2000 eruption. The news says that since the year 2006 there has been more magma in Hekla magma chamber then before the last eruption in the year 2000. This has not meant an eruption so far. Hekla volcano magma chamber have the depth of around 10 to 20 km. This means this inflation that is now taking place does not appear clearly on the surface, but changes are being measured by GPS system that Icelandic Meteorological Office has. This is also appearing on GPS instruments that geological department University of Iceland has. Even if inflation is now more in Hekla volcano then during the eruptions in the year 1991 and 2000 it does not mean that next eruption is going to be bigger. Since the size of the eruption depends on how much of the magma is mobile in the magma chamber. That amount remains unknown until eruption takes place and even then not all of the mobile magma might erupt.

It is also pointed out in the news that it is risky to go on top of Hekla volcano as is. At least while no eruption has taken place currently. Since the risk of eruption is in place and the time from magma starts to move and until eruption takes place is short. Often less then 1 hour. It is advised in this news that people should not go on top of Hekla volcano. The risk is that eruption starts and trap people on top of the volcano, with deadly consequences.

It is possible to read the Icelandic news here. Please use Google Translate with care. It’s not always correct.

Kvikusöfnun meiri í Heklu en árið 2000 (mbl.is)

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March 14, 2014March 14, 2014

Increasing conductivity in Skeiðará glacier river (Grímsfjall volcano)

Since 20-January-2014 there has been increase in conductivity in Skeiðará glacier river that comes from Vatnajökull glacier. The reason for this change is that water is leaking from Grímsfjall volcano. Water levels have also been increasing and dropping during this time since this started.

The conductivity in Skeiðará glacier river from 20-January-2014. Picture from Icelandic Meteorological Office Facebook page. Copyright of this image belongs to Icelandic Meteorological Office.

Conductivity is now measured at 416 µS/cm and according to Icelandic Meteorological Office that is an high value coming from Grímsfjall volcano. This water also goes trough several lakes and before it reaches the sensor at Gígjukvísl bride. So at the source of Skeiðará glacier river this value is probably even higher. No major earthquake activity and no harmonic tremor activity has taken place following this water leak from Grímsvötnum glacier lakes. But it appears that some glacier quakes might be taking place at the moment. Such activity can be seen here on IMO website. Currently the volume of water in Grímsvötn glacier lakes is small since the eruption that took place in Grímsfjall volcano in the year 2011. Coverage of that eruption can be found here. At current time nothing more is expected to happen.

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March 3, 2014

Three earthquakes in Hekla volcano system

Today (03-Mars-2014) three earthquakes where detected in Hekla volcano system. All three earthquakes where small with none having magnitude above 1,0.

The earthquakes in Hekla volcano system. Copyright of this image belongs to Icelandic Meteorological Office.

No other change has been detected in Hekla volcano at this time. Earthquake activity has been taking place in Hekla volcano in the past. It is not clear what is the source or why this earthquake activity is taking place. It is possible to watch Hekla volcano here on my webicorders and live images can be found here. If something happens, but I think it is unlikely to do so at present time.

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February 25, 2014February 25, 2014

Deep earthquake in Hamarinn volcano

Today (25-February-2014) at 09:49 UTC an deep earthquake took place in Hamarinn volcano (is under Bárðarbunga volcano at GVP database as Loki-Fögrufjöll). This earthquake had the depth of 29,6 km and magnitude of 1,8. This means it was created by magma movement rather then tectonic forces.

The earthquake that had the depth of 29,6 km is located 12,5 km south of Hamarinn (64,417 -17,605). Copyright of this image belongs to Icelandic Meteorological Office.

Hamarinn volcano last erupted in July 2011 [coverage of that can be found here] in an minor eruption that lasted for few hours but resulted in glacier flood in the area. Since then activity has dropped, but over the recent months it has been picking up again slowly. So far it is just earthquakes at depth. Harminn volcano is highly active volcano, even if it is not constantly erupting at the moment. The reason is that it is almost centre above the hot spot fuels the eruption activity in this area.

Blog post updated at 21:28 UTC.

February 17, 2014

Minor earthquake swarm in Katla volcano

Over the past two days minor earthquakes have been taking place in Katla volcano. This is just minor earthquake activity. None of the earthquakes so far have reached the magnitude 1,0 that I know of.

Earthquake activity in Katla volcano. Copyright of this image belongs to Icelandic Meteorological Office.

What is interesting about this earthquake activity is that it is taking place inside the caldera of Katla volcano and it is taking place in high winter. When earthquake activity is normally low. What this means is unknown as is and I do not think an eruption is imminent in Katla volcano. This activity is however something to keep an eye on. Since Katla volcano is known to have erupted as early in May. Last such eruption took place in the year 1721 and lasted until October that same year (+-45 days). It is not known if eruptions can take place earlier, I am not going to rule it out even if it is not documented in historical documents about past eruptions in Katla volcano.

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February 17, 2014

Minor earthquake swarm in Hengill volcano

Yesterday (16-February-2014) an minor earthquake swarm took place in Hengill volcano. This earthquake swarm took place because Orkuveit Reykjavíkur (OR) was pumping down water from hydrothermal processing in this part of Hengill volcano.

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

This type of earthquakes happen regularly when Orkuveita Reykjavíkur pumps water down into the ground at this location. At the moment this is just making minor earthquakes. This type of earthquake swarm only last during the period when water is being pumped down into the ground. Once that process is stopped the earthquake activity stops almost immediately.

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February 6, 2014February 6, 2014

Minor earthquake swarm in Geysir volcano and Presthjúkar volcano

Yesterday (05-February-2014) an minor earthquake swarm took place in Geysir volcano (no GVP information) and in Presthnjúkar volcano. None of the earthquakes where above the magnitude of 2,6. The largest earthquakes did appear on my geophone network and were (are for the next few hours when this is written) visible on my webicorders website.

Earthquake activity in Presthnjúkar volcano and Geysir volcano. Copyright of this image belongs to Icelandic Meteorological Office.

Other than this minor earthquake swarm it remains quiet in Iceland. I am not sure why that is at current time. This is the longest quiet period that I remember for the past 5 years at least.

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January 21, 2014

Waiting for the eastern Skaftá glacier cauldron

The glacier flood in Skaftá glacier river is almost over or is over at present time (21-January-2014). This however does not mean that everything is over. Since there are two cauldrons in the Vatnajökull glacier in the Hamarinn volcano it means there is more water stored there now then has now flooded from the glacier. It is now clear that the eastern Skaftá glacier cauldron in Vatnajökull glacier has not emptied it self in this flood from the western Skaftá glacier cauldron.

The eastern (Eystri) and western (Vestari) cauldrons in Vatnajökull glacier. Copyright of this image belongs to Icelandic Meteorological Office.

When the eastern glacier cauldron empties it self they are expecting a lot larger glacier flood to take place. Since there is a lot more water holding up in the eastern Skaftá glacier cauldron. It is also longer since it flooded and emptied it self. Last glacier flood from the eastern Skaftá glacier cauldron was in the year 2010. More information on how this flood system works can be found here (in Icelandic) on Icelandic university website geology department.

January 19, 2014January 19, 2014

Glacier flood started in Skaftár glacier river

It was announced today (19-January-2014) that glacier flood has started in Skaftá glacier river (or connected rivers) from Skjaftár cauldrons in Vatnajökull glacier. Currently the water is discharging from Skaftár cauldrons at the rate of 370 m3/s according to Icelandic Meteorological Office. So far no changes have taken place in harmonic tremors close to Hamarinn volcano where the Skaftár cauldrons lie within Vatnajökull glacier.

Smell of hydrogen sulphide has been detected by people living close the rivers that the glacier flood is discharging into. There is a considerable risk of poisoning if people get to close the rivers that hold the flood water. It is currently believed that it is the western Skaftár cauldron that is now emptying, that one did empty it self back the in the year 2012. That is however not going to be confirmed until the area can be checked by flying over it and see what is taking place at this location. That might take few days since it is dependent on weather when it is possible to do such flight.

Location of Skaftár cauldrons in Vatnajökull glacier. Copyright of this image belongs to Icelandic Meteorological Office. Picture is taken from Icelandic Meteorological Office Facebook page.

The current flood in Skaftár glacier river. The water monitoring stations around Vatnajökull glacier. Red stations are monitored for floods, black ones are normal flow stations. Copyright of this image belongs to Icelandic Meteorological Office. Picture is taken from Icelandic Meteorological Office Facebook page.

Uncertainty level has been declared in the area do to this glacier flood by the Civil Protection and Emergency Management in Iceland. It is advised against people travelling in the area while this glacier flood takes place. On Vatnajökull glacier there is also a risk of new cracks forming in the glacier was the cauldron is emptied of water in the next few days. This cracks are dangerous and really deep and wide on the top, but get narrower closer to the end of them. It is possible to monitor the glacier flood here on Icelandic Meteorological Office website.

Icelandic news about this. Some English text is in some of the news. It is possible to use Google Translate on this, but result can be unreliable.

Skaftárhlaup er mjög líklega hafið (Rúv.is, maps, English text)
Skaftárhlaup hafið en það vex óvenju hægt (Rúv.is, Icelandic, maps)
Óvissustig vegna Skaftárhlaups (Rúv.is, Icelandic, maps)

Skaftárhlaup er hafið (mbl.is, English text)
Óvissustig vegna Skaftárhlaups (mbl.is, Icelandic)
Fundað um næstu skref (mbl.is, Icelandic)

Post updated at 20:34 UTC on 19-January-2014.

January 15, 2014January 15, 2014

Increased conductivity continues in Múlakvísl glacier river (Katla volcano)

Last week I wrote about increased conductivity in Múlakvísl glacier river that comes from Mýrdalsjökull glacier (Katla volcano). This trend has continued into second week with the conductivity. The conductivity in Múlakvísl is now on the range of ~327 to ~360 µS/cm. There has also been a slight increase in water levels following this change in Múlakvísl glacier river. Normal value for this time of year according to Icelandic Meteorological Office is ~180 µS/cm in Múlakvísl glacier river. Since 31-December-2013 the conductivity in Múlakvísl glacier river has always been over 220 µS/cm.

Conductivity in Múlakvísl glacier river. Top: conductivity. Middle: Harmonic tremor. Bottom: Windspeed. Copyright of this image belongs to Icelandic Meteorological Office.

Animated image from Icelandic Meteorological Office showing changes in Múlakvísl glacier river during this time period. Original image can be found here. Copyright of this image belongs to Icelandic Meteorological Office.

No harmonic tremors or earthquakes have been detected (besides normal activity) following this changes. What is taking place is that a cauldron in Mýrdalsjökull glacier is now leaking melt water that has been built up due to hydrothermal (hot springs) activity under the glacier. So far it does not appear that current changes in Múlakvísl glacier river mean anything at all. If that is going to change is impossible to know at this point.

Icelandic News about this

Rafleiðni há en enginn órói mælist (mbl.is)

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Post updated at 19:09 UTC on 15-January-2014.
Post updated at 20:49 UTC on 15-January-2014.

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