Minor earthquake swarm on Tjörnes Fracture Zone (east of Grímsey island)

Today (25-March-2021) a minor earthquake swarm took place east of Grímsey island. Earthquake swarms are common in this area. Largest earthquake in this swarm had a magnitude of Mw3,0. This earthquake swarm might not be over.

earthquake activity east of Grímsey island. Green star shows one earthquake with magnitude 3. Few red dots show smaller earthquakes
The earthquake activity east of Grímsey island. Copyright of this image belongs to Icelandic Met Office.

Earthquake activity in the Tjörnes Fracture Zone often starts slowly before increasing. I don’t know if that is going to happen now since this area has been having a lot of earthquake activity in recent months.

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Moving Iceland geology to a bigger server

Because of current high traffic to this website I plan on moving it to a slightly larger server in the time between April to June. I am not sure yet when I can afford the change since this is a slightly more expensive option at 79€ a month from current price of 9,5€ a month (I also have other websites here that I won’t move since they get little to no traffic at all). I am also expecting far higher traffic to this website in the future when other Icelandic volcanoes start to go active for a long and short time period.

Update on the eruption in Geldingadalur on 22-March-2021

This is a short article about the eruption in Geldingadalur. The volcano that is erupting continues to be Krýsuvík-Trölladyngja volcano system. This might change at later date. This article is written on 22-March-2021 at 17:30 UTC.

  • The eruption is now mostly just in one crater. There is some activity in two other craters but it seems to be getting smaller as the eruption goes on.
  • This eruption is tiny and one of the smallest eruption observed in Iceland.
  • There is risk of new eruption opening up once this eruption ends or starts to get close to ending.
  • There is a fissure in the ground on the right side of the main crater (as seen on the web camera). A lot of volcanic gas comes from that fissure but no eruption has taken place so far.
  • There has not been any noticeable deflation according to GPS data from today (22-March-2021).
  • The main crater is now estimated to be 30 meters high but it is unstable and collapses often.
  • The lava is estimated going to fill Geldingadalur valley in 10 to 14 days if the eruption continues this long.
  • Earthquake activity has almost stopped on Reykjanes peninsula after the eruption started. Once the eruption stops earthquake activity might increase again.

 

The Geldingadalur valley seen from above with Google Earth. Small valley with small mountains on most sides.
This is a image from Google Earth and shows Geldingadalur valley that is now being filled slowly with lava. Copyright of this image belongs to Google Earth/Google and other companies that Google has made this image available with its Google Earth program.

The last eruption period on Reykjanes peninsula lasted from the ~700 to the year ~1400. It can be estimated that current eruption period that has now started on Reykjanes peninsula is going to last until the year ~2400 to the year ~2600. During this time shortest time between eruptions is 1 year but the longest time between eruptions might be up to 10 years. How this going to be exactly is a big question but this estimate of mine is based on the limited historical data that I have read somewhere (I no longer remember where that was).

News items with videos

Tower breaks again, lava gushes forth (Rúv.is)

Web cameras now with English text

Live feed from Iceland volcano (Rúv.is)
Live from Geldingadalir volcano, Iceland (YouTube)

Rúv has moved the stream to YouTube only.

Beint: Eld­gosið í Fagra­dals­fjalli (mbl.is, this camera is on the other side compared to the Rúv camera)

Update at 23:57 UTC

According to the evening news on Rúv the lava and magma that is now flowing into the valley of Geldingadalur is around 1200C and is a primitive magma of Tholeiitic magma series (Wikipedia). The source of this eruption is a magma chamber with the depths of 17 km to 20 km and the origins of the magma it self is far deeper into the hotspot below Iceland. This magma has a lot of CO and CO2 gases that are highly dangerous. There is also a lot of SO2 gas in the eruption and that is dangerous gas.

News in Icelandic about this

Hraunkvikan sýnir beintengingu við miðju möttulsins

Rate of updates

Since the eruption is now in stable activity I am going to limit update to if anything major happens. Next update about the eruption should be on Friday 26-March-2021. Other activity in Iceland is going to be reported as normal if anything happens.

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Article updated at 18:32 UTC. New web camera added.
Article updated at 20:50 UTC. Web camera information updated.
Article updated at 23:57 UTC. Information added about the eruption.

Overview of the eruption in Geldingadalur in Fagradalsfjall mountain

This is a short overview of the eruption that is now ongoing in Geldingadalur in Fagradalsfjall mountain area. This is part of Krýsuvík-Trölladyngja volcano system according to latest information. This information might change as the time and more information is collected. This article is written on 20-March-2021 at 02:58 UTC.

  • This is the first eruption in Krýsuvík-Trölladyngja volcano system since the year 1340.
  • The eruption started at 20:45 UTC according to Icelandic Met Office.  The harmonic tremor from the eruption is almost invisible.
  • The fissure is at the writing of this article estimated about to be 1 km long with the direction south-west and north-east.
  • Currently the eruption is small and there is no risk of damage to any infrastructure. Next road (currently closed because of earthquake damage) that might get damaged is 2,5 km distance from the eruption site.
  • This eruption suggests that more eruption might start in different fissures once this eruption is over.
  • The valley that the lava is flowing into might get filled with lava if the eruption lasts long enough. The valley next to it is equally deep so there is no danger of this lava flow.
  • The eruption is in a area that is difficult to access even by a car.

 

The earthquake activity in the dyke between Fagradalsfjalls and Keili. Mostly just minor eartquakes show by red dots
The earthquake activity in the dyke. Copyright of this image belongs to Icelandic Met Office.

The eruption might only last for two to three days as it currently looks but that might change without warning since it is impossible to know for sure what is going to happen next with this eruption.

There are no good web cameras of this eruption since it is remote and started late on Friday night and the weather on Reykjanes peninsula is not good for today (20-March) or tomorrow (21-March).

Updated at 04:49 UTC. Web cameras added to this article.

Rúv – Beint vefstreymi af eldgosinu – Vogastapi
Beint vefstreymi frá eldstöðvunum – Rúv.is – New! This web camera is closest to the eruption.
Road camera 1
Live from Iceland – Keilir
Live from Iceland – Reykjanes

Article updated at 03:49 UTC. Information added. Spell check fixes.
Article updated at 04:52 UTC. Web cameras added.
Article updated at 14:44 UTC. New web camera added from Rúv.

Eruption confirmed in Fagradalsfjall mountain

This article is going to go get updated soon as possible or a new article is going to be written. This information is going to get outdated quickly. This is Krýsuvík-Trölladyngja volcano.

This volcano eruption seems to have started without any earthquake activity or major harmonic tremor as of writing of this article. More information later this evening.

Update at 22:46 UTC

Here is a web camera link from Rúv. It might work. But all the web cameras are getting heavy traffic now.

Update 22:56 UTC

This is the possible location of the eruption based on satellite images of the area. This is in eastern side of Fagradalsfjall mountain. This is from Icelandic Met Office.

Update at 23:13 UTC

This the first picture of the eruption. The fissure is about 200 meters long at the writing of this article. Picture is from Icelandic Met Office.

Update 00:05 UTC on 20-March-2021

Video of the eruption. Video from Icelandic Met Office. Downloaded from Twitter.

Update at 00:56 UTC on 20-March-2021

Here is a new video of the eruption on Rúv website.
Title of the article was also fixed.

Inflation slows in Krýsuvík-Trölladyngja volcano system

This is a short article that because the situation can change without warning and article is written on 19-March-2021 at 21:07 UTC. There have been updates to names used and now Krýsuvík-Trölladyngja name is used by Global Volcanism Program and Icelandic Met Office. Suggesting that the magma that is about to erupt has its origin in Krýsuvík volcano system eat of current centre of activity. This sometimes happens in Iceland when magma travels long distances deep underground.

Earthquake activity in Krýsuvík-Trölladyngja volcano system with two green stars showing two earthquakes with magnitude larger than three
Earthquake activity in Krýsuvík-Trölladyngja volcano system. Copyright of this image belongs to Icelandic Met Office.

Today at 15:01 an earthquake took place with magnitude of Mw3,1. This earthquake has in my view clear signs of magma movement close to the surface as the depth of this earthquake was just 0,1 km (100 meter).

A magnitude 3,1 earthquake that took place. Image shows P wave and a S wave and a long period after the S wave
A magnitude Mw3,1 earthquake that took place today at 15:01 UTC.

This earthquake strongly suggests that magma created it at shallow depth. It has not yet resulted in an eruption but it is a question if this the final sign before an eruption happens. The current quiet time might last up to 2 months but it is impossible to know for sure.

Earthquake swarm in Reykjanes volcano early morning of 19-March-2021

At 04:30 this morning (19-March-2021) an earthquake swarm started just off the coast of Reykjanestá. This activity looks tectonic in nature for now but it is highly focused in one location. This earthquake activity did start on 24-February-2021 when the Mw5,7 earthquake happened. This activity was only going on for short period of time on 24-February-2021 before it stopped until now.

Earthquake activity in Reykjanes volcano off the coast of Reykjanestá shown by few green stars. A lot of earlier activity is in Fagradalsfjall mountain area.
Earthquake activity in Reykjanes volcano off the coast of Reykjanestá in the far left corner of this image. Copyright of this image belongs to Icelandic Met Office.

Largest earthquakes in this swarm had a magnitude of Mw3,7 but in total of 10 earthquakes with magnitude above 3 took place in this earthquake swarm. Around 100 earthquakes where recorded at the writing of this article but after 06:00 this earthquake swarm slowed down from its peak activity around 05:50. This earthquake swarm might increase again without warning.

Update on the activity between Keilir and Fagradalsfjall mountains

This is a short article written on 17-March-2021 at 17:49 UTC. The situation can change without warning.

It has been less activity in in Fagradalsfjall volcano (Krýsuvík volcano). Current day to day change is not a lot at the writing of this article but it is also possible that bad weather that is now passing over Iceland is masking some of the smaller earthquakes in the dyke between Keilir mountain and Fagradalsfjall mountain. Inflation continues at what seems to be about the same rate as yesterday (16-March-2021).

Earthquake activity shows but less then in last few days. Most of the red dots are located between mountain Keilir and Fagradalsfjall mountain after change in earthquake after the weekend
Earthquake activity in Fagradalsfjall volcano located between Keilir mountain and Fagradalsfjall mountain. Copyright of this image belongs to Icelandic Met Office.

Number of strong earthquakes has dropped after the strong earthquake activity during last weekend (12 to 14 March). What also changed is that the dyke can’t move more south then it already has. It seems that it hit a impasse in the crust that it was unable to break or go around (harder crust is the most common why this happens). The current status is a waiting for the eruption to start and when that happens is impossible to know.

Since there is not a lot of change going on at the writing of this article I am going to slow down the number of updates I am posting. Next update is going to be when something happens or at the latest Monday 22-March 2021.

Web cameras

Beint vefstreymi af skjálftasvæðinu – Borgarfjall (Rúv.is) If an eruption happens it might be visible hereThis web camera no longer works.
Beint vefstreymi af skjálftasvæðinu – EfstaleitiThis web camera no longer works.
Road camera 1
Road camera 2 (night vision/infrared)
Live from Iceland – Keilir – This web camera is working (I think).

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Article updated on 18-March-2021 at 20:07. Web camera updates.

Inflation continues in Fagradalsfjall mountain, eruption expected close to or in Nátthagi valley

This is a short article because the situation is always changing. This article is written on 15-March-2021 at 21:23 UTC. This article is about Fagradalsfjall volcano but Icelandic Met Office updates go to Krýsuvík volcano so I link to that volcano also.

Between Friday and Monday the activity in Fagradalsfjall volcano was really strong. Several earthquakes with magnitude above Mw4,0 took place and the second largest earthquake took place on Sunday 14-March at 14:15 UTC with the magnitude of Mw5,4. Earlier that day at 12:34 UTC an magnitude Mw5,2 earthquake had taken place. According to the news (Icelandic) over 50.000 earthquakes have taken place since 24-February-2021 when this earthquake activity started (20 days ago). Of those six have been larger than magnitude 5, earthquakes with magnitude between 4 to 5 have been 53 and total of 524 earthquakes with magnitude between 3 to 4. Inflation is now reported to be 20 cm or 10 cm on both sides of the dyke. Eruption is expected to happen close to or in Nátthagi valley soon. When that happens is impossible to know but the magma inflow into the dyke doesn’t show any signs of slowing down or stopping.

A lot of red dots on Reykjanes peninsula showing the earthquake activity in Fagradalsfjall mountain area where the eruption is going to happen. Few green stars showing the largest earthquakes on the map.
Earthquake activity in Fagradalsfjall mountain and nearby area. Copyright of this image belongs to Icelandic Met Office.

It has also been reported that the magma dyke managed to push it self a little more south in the line it had been then compared to Friday according to newest data that scientists have access to. Today (15-March-2021) earthquake activity has been small and slow but after 16:30 UTC it started to increase again but at the writing of this article no major earthquake has happened. It has mostly been small earthquakes taking place.

If anything major happens I’ll post update soon as possible.

Web cameras

Beint vefstreymi af skjálftasvæðinu – Borgarfjall (Rúv.is) Nátthagi valley web camera
Beint vefstreymi af skjálftasvæðinu – Efstaleiti
Road camera 1
Road camera 2 (night vision/infrared)

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Magma dyke seems to have stopped close to Nátthagi valley south of Fagradalsfjall mountain

This article is short because the situation is always changing. This is about the volcano Fagradalsfjall but I have also added Krýsuvík because that volcano is being updated at Global Volcanism Program website. I am not sure currently what volcano is considered active in this make injection. This article is written at 20:39 UTC.

Today (12-March-2021) at 07:43 UTC an earthquake with magnitude of Mw5,0 at 3,7 km depth took place close to Nátthagi valley just south of Fagradalsfjall mountain. Over the last 48 hours 72 earthquakes with magnitude above Mw3,0 have taken place. This earthquake activity is happening at the south end of the magma dyke that has now stopped moving south but continues to expand based on the earthquake activity that is now happening. This is also the location where an eruption might happen without any warning or strong earthquake activity. Eruption out on the ocean is no longer considered a possibility because the magma dyke stopped moving south.

Dense earthquake activity on Reykjanes peninsula in the Fagradalsfjall or Krýsuvík volcanoes. A lot of green stars on the map
The dense earthquake activity in Fagradalsfjall or Krýsuvík volcano. Copyright of this image belongs to Icelandic Met Office.

GPS data shows that inflation remains heavy and has moved some GPS stations up to 120mm over a time period of two weeks. There are no signs of this inflation stopping or slowing down.

Web cameras

Beint vefstreymi af skjálftasvæðinu – Borgarfjall (Rúv.is) If an eruption happens. This camera maybe has the best view
Beint vefstreymi af skjálftasvæðinu – Efstaleiti
Live from Iceland
Road camera 1
Road camera 2 (night vision/infrared)

Next article is going to be on Monday 15-March-2021 if an eruption doesn’t happen or something else major doesn’t happen. I am hoping to get weekend break this weekend. If that is going to be successful is currently unclear.

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Strong earthquakes west of Grindavík village and update on magma dyke movements

This is a short article about the activity in Fagradalsfjall volcano. This article is written on 11-March-2021 at 17:34 UTC.

This morning at 08:53 UTC an earthquake with magnitude of Mw4,5 took place west of Grindavík town. Second earthquake with magnitude of Mw3,2 took place at 09:03 UTC. This earthquakes are not connected to any magma movement in this location. The reason for this earthquake activity is because of the inflation from the Fagradalsfjall volcano dyke. According to new measurements the dyke in Fagradalsfjall volcano is moving around 500 meters every 24 hours. Currently the dyke has moved more south but it was moving south-west yesterday and the days before that. Today (11-March-2021) the dyke has only 2 to 3 km left until it goes under the ocean and a road called Suðurstrandarvegur (road 427). If the magma reaches the ocean and an eruption starts, it is going to be an explosive eruption while the ocean can access the main craters that are erupting. Depending on locations this can go on for weeks and is going to form new islands that might only exist for short time period until the ocean erodes them away.

Dense earthquake activity on Reykjanes peninsula in the volcano Fagradalsfjall. Three green stars west of Grindavík town and a lot of red dots showing new earthquake activity.
Earthquake activity in Fagradalsfjall volcano. Copyright of this image belongs to Icelandic Met Office.

If an eruption happens before the magma dyke reaches the ocean the magma only has 2 to 3 km left until it reaches the ocean and it is now expected if that happens that the lava is going to reach the ocean in 6 to 10 hours and go over Suðurstandarvegur (road 427). Since 24-February-2021 over 34.000 earthquakes have been recorded by Icelandic Met Office in this volcano activity.

Web cameras

Beint vefstreymi af skjálftasvæðinu – Borgarfjall (Rúv.is) New!
Beint vefstreymi af skjálftasvæðinu – Efstaleiti (Rúv.is)
Road camera 1
Road camera 2 (night vision/infrared)
Live from Iceland