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Nye sprækker nær udbrudsstedet i Geldingadalir

5.4.2021

Opdateret 08.04 12:25

Lavastrømmen fra den seneste udbrudssprængning synes for det meste at strømme ned i Geldingadalir. Denne tredje udbrud revne åbnet ved midnat på den 6. ^th af april og er mellem de to eksisterende sprækker. Redningshold fra den islandske Association for eftersøgning og redning havde opdaget nedsynkning i området på 6. ^th april cirka 420 meter nordøst for den oprindelige udbrud område i Geldingadalir, som var omkring 150 m lang og ca. 1 meter dyb.

I de billeder, der blev taget under rekognoscering flyvning på 7. ^th april kan det ses, at felterne lava fra de tre eruption sprækker nu fusionerer. Lava fra det tredje revne er strømmet sydpå ind i Geldingadalir og nordøst mod udbrudsstedet over Meradalir. Der er et kontinuerligt lavafelt mellem de tre udbrudsområder, som faktisk hører til den samme vulkanske revne over magma-indtrængen ved Fagradalsfjall.

 

Et kontinuerligt lavafelt mellem de tre udbrudssteder ved Fagradalsfjall. (Foto: Almannavarnir / Björn Oddsson)

Oversigtskort, der viser placeringen af ​​de tre udbrudssteder i rødt og lavastrøm fra dem, som situationen var den 7. april. Lavastrømningen fra den sidste revne er ikke kortlagt nøjagtigt. Lavas omrids er tilnærmet fra luftfoto af regionen.

Opdateret 05.04 kl. 15:40

Fotos af to nye vulkanske sprækker tæt på det oprindelige udbrudsområde i Geldingadalir, der ligger ca. 700 meter NØ for kraterne i Geldingadalir. De nye revner er i alt 200 meter lange. Lavaen fra sprækkerne er ikke tyktflydende og flyder hurtigt i en smal lavaflod ind i Meradalir-dalen, øst for de nye sprækker, hvor der dannes et nyt lavafelt. 

Fotos: Björn Oddsson / Institut for Civilbeskyttelse og Nødstyring

Opdateret 05.04 kl. 14:15

En ny ekstra spalte åbnede ca. 12:00 i dag nær det oprindelige udbrudssted i Geldingadalir. De første skøn over revnens længde er ca. 200 meter, og midten af ​​sprækket er ca. 1 kilometer NØ for udbruddet i Geldingadalir. Lavaen fra den nye revne strømmer mod Meradalir-dalen øst for den nye revne.

Helikoptere fra den islandske kystvagt er ved det nye udbrudsområde for at sikre, at området evakueres. En flyveplads med forskere er på vej mod sprækket for mere nøjagtigt at vurdere placeringen og størrelsen af ​​den nye revne.  

På grund af manglen på aske og tefraemission i atmosfæren forbliver luftfartskodekoden for Keflavik lufthavn orange, da der ikke er nogen overhængende fare for luftfarten.

En live stream fra den nye revne kan ses på RUV 2 . 

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Et mindre udbrud i gang

Se IMO’s Twitter-konto for de seneste oplysninger om jordskælv. @Vedurstofan

Opdateret 29.3 kl. 09:30

Civil Protection and Emergency Management’s Science Board holdt et møde fredag (Mars 26.) for at drøfte vulkanudbruddet i Geldingadalir på Reykjanes-halvøen. Der er indsamlet en masse data, herunder målinger på stedet og fjernmålinger sammen med modelleringsarbejde, der forudsiger begivenhedens mulige adfærd i de kommende dage. En rapport med en detaljeret beskrivelse af arrangementets generelle status og forslag til regelmæssig overvågning vil blive frigivet om kort tid.
Både det islandske metkontor og Islands Jordvidenskabelige Instituts Universitet poster jævnligt resultater, og folk opfordres til at se deres websider, twitter-streams og Facebook-sider.

Vulkanudbruddet i Geldingadalir har nu været i gang i ni dage. Lavaen er basaltisk og meget flydende med lidt eksplosiv aktivitet. Det er et meget lille udbrud, og lavastrømmen har været stabil ved 5-7 m3/s siden starten. I øjeblikket er omfanget af lavafeltet inden for Geldingadalur, men hvis udbruddet fortsætter i samme tempo, er det modelleret, at lavaen vil flyde østpå mod Merardalur-dalen. Hvis vulkanen fortsætter med at bryde ud, kan det i sidste ende ende med at blive kategoriseret som et skjold vulkan. Shield vulkaner er generelt dannet over lange perioder med lava felter strækker sig fra et par til flere kilometer omkring kilden. Der er ingen måde at fortælle, hvor længe udbruddet vil vare.

Den nuværende magma er rig på MgO (8,5%) hvilket indikerer, at det er fra dybder på omkring 17-20 km. Der har været konstant gasforurening tæt på eruptionstedet, rumligt bestemt af lokale vindforhold. Gasser kan ophobes til livstruende niveauer under visse vejrforhold. Der har ikke været tegn på væsentlige tektoniske bevægelser siden udbruddet startede. Der er i øjeblikket ingen tegn på nye åbninger andre steder langs magma injektion sti.

Dette udbrud kræver specifik og målrettet overvågning af selve udbruddet og også af gassens indvirkning på luftkvaliteten og vindretningen.

 

Uptdated 23,3 kl 12:38

Faldende SW-ly vind i dag og usund luftkvalitet kan forventes i nærheden af eruption site efter 19:00 i dag. SO2 koncentration tæt på vulkanen kan overgå over 9000 μg/m3, og CO2 kan også samles i dale i landskabet. Det anbefales at forlade området før kl. 17.00, holde sig væk fra dale og følge den markerede sti.

Opdateret 21.03. 17:25

Det islandske met Office overvåger nøje udviklingen af gasforurening fra udbruddet i Geldingadalur. Gasforurening fra vulkanerne forventes ikke at have en væsentlig indvirkning på beboernes trivsel og sundhed på Reykjanes-halvøen og hovedstadsområdet i de næste par dage. Vejr, vindretning og forurenende stoffer (såsom SO2 og CO2) fra vulkanudbruddet påvirker alle styrken og fordelingen af gasforureningen.

Den islandske Met Office har udarbejdet en prognose model, der forudsiger den sandsynlige fordeling og koncentration af gasforurening på grund af udbruddet i Geldingadalur. Prognoserne opdateres to gange om dagen.

Opdateret 21.03 13:40

Det videnskabelige rådgivende udvalg for den islandske civilbeskyttelse mødtes i går eftermiddags den 20. marts for at evaluere den seneste udvikling af vulkanudbruddet i Geldingardalur på Reykjanes-halvøen. Konklusionen på mødet var, at følgende udviklinger er mulige:

• Udbruddet vil falde gradvist og ende i de kommende dage eller uger.
• Nye vulkanske sprækker kunne åbne på eruption site eller langs magma diget tæt på Mt. Fagradalsfjall.
• Sandsynligheden for et stort jordskælv tæt på Mt. Fagradalsfjall er reduceret på grund af den igangværende vulkanske aktivitet.
• Et jordskælv op til størrelsesorden 6,5 kunne udløses i Brennisteinsfjöll vulkanske system, der ligger øst for Mt. Fagradalsfjall.

Det videnskabelige rådgivende udvalg for den islandske civilbeskyttelse advarer om farer i området omkring eruptionstedet.

Det er vigtigt at huske på, at nærheden af eruption site er farligt som pludselige ændringer kan forventes. Det videnskabelige rådgivende udvalg for den islandske civilbeskyttelse skitserede følgende farer tæt på det igangværende udbrud:

Nye vulkanske sprækker kunne dannes i området uden varsel.

• Glødende lavastykker kan falde ned fra kanterne af lavafronten, og pludselige lavaudbrud kan forventes, hvor nye lavatunger finder vej ud af lavastrømmen. Dette kan ske meget hurtigt, hvilket gør det vanskeligt for folk at komme ud af vejen, selv når de kører.
• De vulkanske kratere er nu flere meter høje og kan derfor være ustabile og smuldre uden varsel med de konsekvenser, at lavastrømmen pludselig kan ændre retning.
• Eksplosioner kan ske, hvor lavaen strømmer over vand-logget jorden, hvilket resulterer i lava bliver kastet i forskellige retninger.
• Lavaen strømmer ind i en lukket dal. Derfor kan dødelige vulkanske gasser, hvoraf mange er tungere end luft, ophobes i lavtliggende områder. Faren stiger i rolige vejrforhold.

IMO fortsætter med at overvåge gasspredning fra udbruddet. Det er usandsynligt, at gasforureningen vil påvirke mennesker, der bor i hovedstadsregionen og byerne på Reykjanes-halvøen i de kommende dage, alvorligt. Vejrforholdene og koncentrationen af gasser (f.eks. Den seneste prognose for spredning af gas er tilgængelig øverst på IMO’s websted, en.vedur.is.

Opdateret 20.03 13:45

Hvad vi ved indtil videre

Omkring kl. 20:45 UTC 19. marts 2021 begyndte et vulkanudbrud ved Geldingadalur, tæt på Fagradalsfjall på Reykjanes-halvøen. Udbruddet blev først set på et webkamera placeret tæt på bjerget. Det blev også bekræftet på termiske satellitbilleder.

Eruption site er i en dal, omkring 4,7 km inde i landet fra den sydlige kyst af halvøen. Kystbyen Grindavík er den tættest befolkede region til eruptionstedet, der ligger ca. 10 km mod sydvest.

Udbruddet betragtes som lille på dette tidspunkt, og den eruptive revne er appr. 200 m lang. Lavaområdet dækker et område, der er ca. 500 m bred og betragtes som mindre end 1 km2. Lava springvand er små og lavastrømme er i øjeblikket en meget lokal fare. Den seismiske aktivitet er mindre og spredt rundt i Fagradalsfjall-området.

The aviation colour code for Keflavik international airport has been lowered to orange as there is no indication of production of ash and tephra and no imminent hazard for the aviation.

Volcanic gas (SO2) has been detected at the source of the eruption. A model for gas dispersion can be seen at the IMO web site. Currently, gas pollution is not expected to cause much discomfort for people except close up to the source of the eruption. The gas emissions will be monitored closely. 

The area of the eruption is considered very dangerous – the eruption site can change without notice and put people at risk unexpectedly.

Reykjanesbraut – the main road from the capital region to Reykjanesbær and the international airport at Keflavík is open. However, Suðurstrandarvegur – the road along the south coastline of Reykjanes peninsula is closed between the two coastal towns Grindavík and Þorlákshöfn. Other roads and unpaved tracks in the vicinity of the eruption site are also closed. 

Updated 20.03 11:10

The eruption is considered small at this stage and the volcanic activity has somewhat decreased since yesterday evening. The eruptive fissure is appr. 500 – 700 m long. The lava area is less than 1 km² covering an area that is appr. 500 m wide. Lava fountains are small and lava flows are currently a very local hazard. The seismic activity is minor and spread around the Fagradalsfjall area. There is no indication of production of ash and tephra and currently gas pollution is not expected to cause much discomfort for people except close up to the source of the eruption. The gas emittions will be monitored closely. 

The aviation color code for Keflavik international airport has been lowered to orange as there is no indication of production of ash and tephra and there is no imminent hazard for the aviation.

Reykjanesbraut – the main road from the capital region to Reykjanesbær and the international airport at Keflavík is open. However, Suðurstrandarvegur – the road along the south coastline of Reykjanes peninsula is closed between the two coastal towns Grindavík and Þorlákshöfn. Other roads and unpaved tracks in the close vicinity of the eruption site are also closed.

Updated 19.03 23:20

At around 20:45 UTC today, 19 March, a volcanic eruption began at Geldingadalur, close to Fagradalsfjall on the Reykjanes Peninsula. The eruption was first seen on a web camera positioned close the mountain. It was also confirmed on thermal satellite imagery. At the time of writing, the weather on the peninsula is wet and windy, and an orange glow can be seen in low clouds on the horizon from Reykjanesbær and Grindavík. The eruption site is in a valley, about 4.7 km inland from the southern coast of the peninsula. The coastal town of Grindavík is the closed populated region to the eruption site, located approximately 10 km to the southwest.

Earthquake activity in the region of the magma intrusion has been lower in recent days, and there is presently no intense seismicity occurring in the region. Earlier in the day, several low-frequency earthquakes were recorded below Fagradalsfjall. There are presently no reports of ash fall, although tephra and gas emissions are to be expected. In line with well-rehearsed contingency plans, the aviation colour code for the Reykjanes Peninsula has been elevated to red, signifying an eruption in progress. Additional domestic restrictions have been put in place, including the closure of Reykjanesbraut – the main road from the capital region to Reykjanesbær and the international airport at Keflavík.

Updated 18.03 at 11:33

About 400 earthquakes have been detected between midnight and seven AM on the Reykjanes peninsula. This is somewhat less seismic activity in comparison to previous mornings where the numbers have been around 1,000 earthquakes. 

Yesterday around 1400 earthquakes were detected. Three were larger than magnitude 3, the largest M3.3 at 2:37AM located around 1km N of Nátthagi valley. 

Today at 13:00GMT the Scientific Advisory Board of the Icelandic Civil Protection will meet to evaluate the latest monitoring data. Findings of the meeting are expected shortly after 15:00GMT.

Updated 15.03 at 11:00 

Since midnight over 1000 earthquakes have been detected on the Reykjanes Peninsula, with the most active area located south of Mt. Fagradalsfjall. The largest earthquakes measured at M3,2, at 01:20 GMT last night and 07:39 GMT this morning.

Yesterday, March the 14^th, over 3000 earthquakes were detected in the Reykjanes Peninsula. The largest earthquake measured M5,4 at 14:15 GMT. Yesterday evening four earthquakes measuring M3,3-M3,6 were detected, three of which were located by Mt. Fagradalsfjall and the fourth northwest of Grindavík village. 

Updated 11.03 at 16:00

Over 1700 earthquakes have been measured in the Reykjanes Peninsula since midnight, few of which were over M3, the largest one measured M4,6 at 08:53 GMT this morning. As before, the magmatic activity is centered around Mt. Fagradalsfjall southwest of Mt. Keilir. 

Yesterday, March 10th, 2500 earthquakes were detected in the Reykjanes Peninsula, 40 of which were over M3, the largest one measuring M5,1 at 3:14 GMT.

Yesterday, the Scientific Advisory Board of the Icelandic Civil Protection met to discuss the latest monitoring results from the seismic unrest on the Reykjanes Peninsula. The main findings of the meeting were:

• The dike intrusion is expanding with the most active magma flow centered at the southern part of it. A volcanic eruption remains a possibility as magma is still flowing into the corridor. With the ongoing activity the probability of an eruption increases day by day. It is considered very unlikely that lava from a possible eruption would reach populated areas.
• It is important to follow the activity in the southern region of Mt. Fagradalsfjall in order to evaluate whether the dike is expanding to the south. 
• Latest satellite images and GPS data show that accumulation of magma is concentrated at the southern end of the dike beneath Mt. Fagradalsfjall. This is currently the most likely site for a possible eruption. 
• If the dike keeps expanding and increasing stresses in the area, continuing earthquake activity that can be felt in populated areas is expected. 

Latest satellite images and GPS data show that accumulation of magma is concentrated at the southern part of the dike beneath Mt. Fagradalsfjall. This is the most likely site for a possible eruption. InSAR image reflects changes between March 3 to March 9 2021. Image contains modified Copernicus Sentinel data [2021]

Possible eruption could begin without strong precursory signals

Currently, the magma is shallow, lying 1-1,5 km beneath the crust. Therefore, it can be expected that an eruption could start without a strong precursory signal, as the magma can easily brake through the last hundreds of meters of the crust once the critical pressure is reached. From experience of lava flow eruptions (as we might expect), the eruption tremor is weak and has a low amplitude. For this reason, the IMO has installed webcams which can be used to monitor the area, in case of an eruption will start without clear precursory signals. 

Updated 09.03. at 12.30

About 5:20 this morning, the activity at Mt. Fagradalsfjall, south of the corridor, increased with a sudden increase in seismic tremor. However, the unrest soon decreased. Magma movements are a likely cause for this activity which is very localized to the south of the magma intrusion. The tremor is an indication that the intrusion is expanding. 

Variable levels of seismic tremor are to be expected during such periods of seismic unrest. Therefore, it is likely that there will be periods of intense tremor interspersed with less intense activity over the coming days. A volcanic eruption remains a possibility. Therefore, scientists and civil protection staff are on alert, and they are ready to respond to a range of situations, including damaging earthquake activity or a volcanic eruption.   

Possible development is as follows: 

• The ongoing seismic activity reduces in the coming days and weeks. 

• The seismic swarm will increase in intensity, possibly with an earthquake up to magnitude magnitude 6 in the area. 

• An earthquake up to magnitude 6.5 could be triggered in a nearby volcanic system, roughly 20 km east of the current location of the activity. 

• Magma intrusions continue, resulting in: 

  • An eventual decrease in magma inflow, resulting in the magma solidifying in place without an eruption. 

  • An effusive volcanic eruption could occur, resulting in lava flows that should not threaten inhabited areas of the peninsula.
    

Click here to view alarger image or to download the picture. This picture shows the location where the magma chamber is forming under the earth’s crust. When magma flows into the sedimentary strata and forms magma tunnels, as is currently the case in the area of unrest between Keilir and Fagradalsfjall, pressure is formed in the earth’s crust. This creates tension on the east and west sides of the area of unrest.

Updated 03.03. at 19.00

At 14:20 today a sudden increase in seismic tremor was detected throughout most of Iceland’s national seismic network. At the time of writing, the tremor continues although its intensity has reduced slightly. The tremor, which comprises many small, overlapping earthquakes, is sourced from a region 2 km southwest of Keilir on the Reykjanes Peninsula. Similar bursts of tremor have been observed ahead of previous volcanic eruptions in Iceland. Magma movements are a likely cause for the ongoing signal, and it is possible that an effusive (lava-producing) eruption could occur close to Keilir. However, at the time of writing, no volcanic eruption is occurring on the Reykjanes Peninsula.

Analysis of various sensor and satellite-based monitoring data continues at pace, with further spaceborne radar images becoming available late this evening. As a precaution for domestic and international air travel, the volcanic aviation colour code for the Reykjanes Peninsula has been elevated from yellow (elevated unrest) to orange (heightened unrest). The orange alert represents the third-highest level, with red reserved for an imminent or ongoing volcanic eruption.

Updated 03.03.

On 1 March, the Scientific Advisory Board of the Icelandic Civil Protection met to discuss the latest monitoring results from the seismic unrest on the Reykjanes Peninsula. In particular, the latest satellite-based radar (InSAR) image was reviewed. The displacements in the InSAR scene show more ground deformation than can be explained by the earthquake activity alone. The most likely explanation is that magma intrusions are occurring close to Fagradalsfjall, where the earthquake activity has persisted in recent days. The latest satellite results will be processed with additional geodetic modelling to better understand the causes of the ground deformation.

Given the new results discussed by the Scientific Advisory Board, it is important to consider scenarios in the development of the seismicity that could involve volcanic activity close to Fagradalsfjall.

Possible developments

• The ongoing seismicity reduces in the coming days and weeks.
• The seismic swarm will increase in intensity, possibly with an earthquake up to magnitude 6 in size nearby Fagradalsfjall.
• An earthquake up to magnitude 6.5 in size could be triggered in the Brennisteinsfjöll mountain range, over 20 km east of Fagradalsfjall.
• Magma intrusions continue in the vicinity of Fagradalsfjall.
  • The intrusive magma movements stop and eventually solidify.
  • An effusive volcanic eruption could occur, resulting in lava flows that should not threaten inhabited areas of the peninsula.

The evolution of the seismicity continues to be monitored day and night, and in the event of an eruption, various contingency plans are in place.

Updated 24.02.

On February 24th 2021, two earthquakes above magnitude M5 were recorded. The larger one, M5.7,  was at 10:05 and at 10:30 a M5.0 was measured. Later that day at 12:37 a M4.8 was recorded. Since the beginning of this unrest 16 earthquakes above  M4 have been recorded and 90 earthquakes above M3. They have been felt widely in the SW part of the country and the larges once in the NW part as far as Ísafjörður. Note that all reviewed earthquakes have occurred on the Reykjanes Peninsula, roughly between Kleifarvatn and Svartsengi. Be aware that our web shows in accurate locations from the automatic system.

Today five earthquakes above M4 have been measured in the northern part of Fagradalsfjall, M4,4 at 12:06, M4,0 at 12:24, M4,1 at 13:51 og M4,2 at 15:10. All those are in a similar location as the M5,7 earthquake. Our interpretation is that these are triggered earthquakes caused by the intense activity and deformation that has occurred in the area. The swarm is still ongoing and roughly 5000 earthquakes have been detected with the automatic system since the beginning of the swarm.

The satellite image below displays a Sentinel-1 interferogram spanning the period 19-25th February. This shows ground deformation associated with the recent earthquake activity on the Reykjanes Peninsula and indicates this was related to a combination of movement on north-south trending faults and left-lateral movement over a large section of the plate boundary (~25 km segment – from Svartsengi to Kleifarvatn).

Red amplitudes represent movement towards the satellite and purple amplitudes movement away from the satellite (path is west of Iceland). The black arrows in the right corner below show the heading and look direction of the satellite. The magnitude 5.7 earthquake that occurred on the 24th February is displayed by the red star. Here is a PDF version of the picture above.

There is no indication in this interferogram for shallow magmatic intrusions, however the inflow of magma from depth cannot be ruled out, as this activity is part of an ongoing volcano-tectonic reactivation of the ReykjanesPeninsula.