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Eyjafjallajökull/Fimmvörðuhálsi eruption opens a new fissure 31 March 2010

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Icelandic broadcaster RUV reports tonight that a new fissure has opened at the Eyjafjallajökull/Fimmvörðuhálsi eruption site. At Fimmvörðuhálsi right now it is (a) getting dark and (b) snowing so it’s hard to get a good webcam picture: this capture from a clear period at around 19:40 GMT is the best I could do. If it is clearer later there should be some spectacular night-time pictures [EDIT: see pictures from 20:08 and 21:46 GMT below).

Eyjafjallajokull fra Fimmvorduhalsi 2010-03-31

The yellow arrow on the left marks the location of the new eruptive fissure, from which incandescence (more dancing fire fountains) can just be made out. The red arrow on the right indicates the main fissure.

EDIT: A picture from slightly later, around 20:08 GMT:

Eyjafjallajokull fra Fimmvorduhalsi 2010-03-31

EDIT: and another, from 21:46 GMT. Positively Dantesque:

Eyjafjallajokull fra Fimmvorduhalsi 2010-03-31

For all our Eyjafjallajökull coverage: Eyjafjöll « The Volcanism Blog.

News
Ný sprunga myndaðist – RUV, 31 March 2010

Information
Global Volcanism Program: Eyjafjöll – summary information for Eyjafjallajökull, which the GVP calls Eyjafjöll (1702-02=)
Eyjafjallajökull eruption March 2010 – summary of events from the University of Iceland’s Nordic Volcanological Center
Photos from Fimmvörðuháls – images and information from the Iceland Meteorological Office

The Volcanism Blog

Eyjafjallajökull/Fimmvörðuhálsi eruption: another satellite image at the NASA Earth Observatory 30 March 2010

Posted by admin in activity reports, eruptions, Eyjafjöll, Iceland, NASA Earth Observatory, volcanoes.
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Eruption of Eyjafjallajokull Volcano, Iceland, 26 March 2010 (NASA Earth Observatory)

Hot on the heels of the Advanced Land Imager’s view of the Eyjafjallajökull eruption showcased by the NASA Earth Observatory a few days ago comes this MODIS image captured by the Terra satellite on 26 March 2010 which shows very clearly the location of the current activity at Fimmvörduháls, between the two icecaps of Eyjafjallajökull (west) and Mýrdalsjökull (east). It is fortunate that the eruption is between the icecaps and not beneath them: a subglacial eruption would threaten to unleash a meltwater flood or jökulhlaup.

Eruption of Eyjafjallajökull Volcano, Iceland – NASA Earth Observatory, 29 March 2010

Meanwhile, the Fimmvörduháls webcam operated by Icelandic telecomms company Míla is providing great close-up images of the eruption once again. Vigorous fire fountain activity is visible even in daylight. This view was captured at 18:28 GMT this evening:

Eyjafjallajokull fra Fimmvorduhalsi 2010-03-30

For all our Eyjafjallajökull coverage: Eyjafjöll « The Volcanism Blog.

Information
Global Volcanism Program: Eyjafjöll – summary information for Eyjafjallajökull, which the GVP calls Eyjafjöll (1702-02=)
Eyjafjallajökull eruption March 2010 – summary of events from the University of Iceland’s Nordic Volcanological Center
Photos from Fimmvörðuháls – images and information from the Iceland Meteorological Office

The Volcanism Blog

Marsili seamount: tsunami threat for Southern Italy? 30 March 2010

Posted by admin in Italy, Marsili, natural hazards, submarine volcanism, volcano monitoring, volcanoes.
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Mount Marsili is a 3000-metre high seamount beneath the Tyrrhenian Sea, 150 km south-west of Naples. Marsili is active and recent research has indicated signs of restlessness (see this 2006 paper in PDF), although the risks of any dangerous eruptive activity are very slight). In an interview with the Italian newspaper Corriere della Sera, the director of the Istituto Nazionale di Geofisica e Vulcanologia (INGV), Dr Enzo Boschi, has reminded everyone that Marsili is active and that there is a potential threat of an eruption/collapse generating a tsunami that would threaten Southern Italy:

It could happen tomorrow. The latest research says that the volcanic edifice is not strong and its walls are fragile. Furthermore we have measured the magma chamber that has formed in recent years and it is of large dimensions. All this tells us that the volcano is active and could erupt unexpectedly.

According to the article, observations indicate that hydrothermal emissions from vents around Marsili have become more intense recently, and evidence of landslides discovered by the oceanographic research vessel Urania last February ‘indicate an instability impossible to ignore’. Dr Boschi warns that a flank collapse at Marsili ’would displace millions of cubic metres of material, which would be capable of generating a wave of great power’. Marsili is currently unmonitored, observes Dr Boschi: ‘A network of seismometers should be installed around the edifice, connected on land to a volcano monitoring centre. But this is beyond the budget’.

And it seems reasonable to suggest that the budget is what this article is actually all about. Despite the new attention this story will bring to Marsili as it gets cut-and-pasted around the web, there is nothing substantially new here, as Aldo Piombino notes in a very comprehensive post published on his blog today. No new activity lies behind this report, and nor has the potential threat, such as it is, changed in any way. The novelty, he observes, is in public attention being drawn to the need to monitor Marsili, which has been invisible in every sense as far as the Italian public is concerned.

Undersea volcanoes tend to be out of sight and out of mind. Writing in 2008, Aldo Piombino called Marsili ’one of the least-known of the huge volcanic systems of Europe’, and argued that more attention must be paid to this active and potentially very destructive underwater giant:

It is statistically very unlikely that in our lifetimes we will see an explosion of Marsili, and even less likely that we will see a tsunami caused by a landslide on its flanks, but it is to be hoped that it will be placed under close seismic and geochemical surveillance, as with other active Italian volcanoes. I believe that it is necessary for civil protection and for science that one of the largest volcanoes in Europe is better understood.

Boris Behncke of the INGV discussed Marsili’s activity in the course of his Q&A on Dr Klemetti’s Eruptions blog last year, but also remarked that monitoring Marsili was not a priority for the INGV [UPDATE: in fact that is not what Boris meant. He meant that Marsili has not been a priority for the Italian authorities, Civil Defence, and the Italian public, rather than the INGV - see his comment at Eruptions]. Dr Boschi’s comments today would seem to indicate that that has changed. Aldo Piombino observes today that the technology is available within the INGV to monitor Marsili directly from the seabed using new broadband seismometers transmitting to land-based monitoring stations, and supports Dr Boschi’s call for full monitoring of the volcano. But that cannot happen without money, which is more likely to be forthcoming if the potential (and real but, it must be emphasized again, very remote) dangers of a tsunami-generating collapse at Marsili are stressed – hence the Corriere della Sera article.

So, it seems that a push has begun within Italian volcanology to get Marsili wired up for continuous and comprehensive monitoring. Let us hope it succeeds.

UPDATE 30 March 2010: Dr Erik Klemetti has more on Marsili at Eruptions, and Boris Behncke, himself of the INGV (Dr Boschi is Boris’s boss), has an illuminating comment here.

News
Torna a far paura il vulcano sommerso nel TirrenoCorriere della Sera, 29 March 2010
Undersea volcano threatens southern Italy: report – AFP, 29 March 2010
Il Monte Marsili, un gigantesco vulcano nascosto dalle profondità del Mar Tirreno – scienzeedintorni, 4 April 2008
Finalmente alla ribalta il più grande fra i vulcani sommersi nel Tirreno, il Monte Marsili – scienzeedintorni, 29 March 2010

The Volcanism Blog

A very Australian volcano at the Royal Botanic Gardens, Melbourne 29 March 2010

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Guilfoyle's volcano, Royal Botanic Gardens Melbourne (illustration copyright RBGM)

History offers surprising connections between gardens and volcanoes, as we’ve reported before here at The Volcanism Blog. From Australia comes news of the restoration of a particularly notable example of the volcano as horticultural feature: Guilfoyle’s Volcano, in the Royal Botanic Gardens, Melbourne. The ‘volcano’ is in fact a reservoir holding 1.3 million litres of water, built and landscaped under the direction of Sir William Guilfoyle, curator of the gardens 1873-1909. The ‘crater’ of the volcano features floating gardens, while the slopes are landscaped with boulders and areas of red stones and succulents simulating lava flows in a modern scheme designed by landscape architect Andrew Laidlaw. The feature had remained unseen and neglected since being fenced off in the 1950s.

[Illustration of Guilfoyle's Volcano, copyright Royal Botanic Gardens Melbourne, reproduced here under the 'fair use' provisions of the Australian Copyright Act 1968.]

The Volcanism Blog

NASA Earth Observatory: cool flows at Llullaillaco 29 March 2010

Posted by admin in Argentina, Chile, Llullaillaco, NASA Earth Observatory, volcanoes.
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Llullaillaco volcano, Argentina-Chile border (ISS astronaut photograph, 9 Dec 2009)

The latest image of the day at the NASA Earth Observatory is this astronaut photograph of Llullaillaco volcano, which is situated on the Argentina/Chile border. Llullaillaco is the highest historically active volcano in the world, 6739 metres high, and last erupted in the nineteenth century. The lava flow extending to the north of the volcano shows very clearly features typical of a viscous flow on a steep slope. Lava at the edges of the flow has cooled more rapidly than that in the centre to produce the walled channel effect of a flow levée, while the faster cooling of the upper surface of the lobe at the front of the flow has produced characteristic layering and pressure ridges at 90 degrees to the direction of the flow. The Earth Observatory caption refers to the lobes of this flow as coulées (but this is what I call a coulée).

It’s also interesting to note, given the time of year, that the head of the Easter Bunny is clearly visible between the two lobes of the lava flow in the top right of the image:

The Llullaillaco Easter Bunny

[Astronaut photograph ISS022-E-8285 was acquired on December 9, 2009, with a Nikon D2Xs digital camera using an 800mm lens, and is provided by the ISS Crew Earth Observations experiment and Image Science & Analysis Laboratory, Johnson Space Center. The image was taken by the Expedition 22 crew.]

Llullaillaco volcano, Argentina-Chile border – NASA Earth Observatory, 29 March 2010

The Volcanism Blog

The fires of Fimmvörðuhálsi 28 March 2010

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A new webcam is providing dramatic live images of the Eyjafjallajökull/Fimmvörðuhálsi eruption, particularly after dark. The images below were captured between 20:55 and 21:00 GMT this evening, when the fire fountains seemed to be particularly vigorous.

Eyjafjallajokull fra Fimmvorduhalsi 2010-03-28 [1]

Eyjafjallajokull fra Fimmvorduhalsi 2010-03-28 [2]

Eyjafjallajokull fra Fimmvorduhalsi 2010-03-28 [3]

Eyjafjallajokull fra Fimmvorduhalsi 2010-03-28 [4]

The webcam is provided by Icelandic telecommunications company Míla, and can be found at this link: Eyjafjallajökull frá Fimmvörðuhálsi. Also available from Míla, the Eyjafjallajökull frá Þórólfsfelli webcam (which is situated further from the seat of the eruption).

UPDATE. The Fimmvörðuhálsi camera has broken down. Oh well, no doubt they will get it fixed in due course.

For all our Eyjafjallajökull coverage: Eyjafjöll « The Volcanism Blog.

Information
Global Volcanism Program: Eyjafjöll – summary information for Eyjafjallajökull, which the GVP calls Eyjafjöll (1702-02=)
Eyjafjallajökull eruption March 2010 – summary of events from the University of Iceland’s Nordic Volcanological Center
Photos from Fimmvörðuháls – images and information from the Iceland Meteorological Office

The Volcanism Blog

March 2010 activity at Concepción, Nicaragua 27 March 2010

Posted by admin in activity reports, Concepción, eruptions, Nicaragua.
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Among the volcanic events that passed unrecorded here during my recent absence through illness was a burst of activity from Nicaragua’s Concepción volcano (which is among the country’s most active volcanoes).

On 8 March an ash and gas plume from Concepción rose to 2,100 metres altitude and light ashfall was reported in nearby communities. Low levels of seismic activity and occasional small explosions producing light ashfall were reported during subsequent days. On 12 March Washington VAAC issued a volcanic ash advisory reporting an eruption producing an ash cloud that reached FL100 (10,000 feet / 3,000 metres altitude). According to news reports there were two further explosions on 14 March. No casualties or damage resulted, although civil defence alerts remained in place for communities around the volcano. The Nicaraguan geological service INETER described the volcano on 19 March as ‘practically in a full eruptive phase’, with 34 explosions between 18:00 on 17 March and 11:45 on 18 March. On 19 March it was reported that the Nicaraguan government was sending army and navy units to the area around Concepción to strengthen civil defence preparations and prepare evacuation routes, ‘just in case’. The location of Concepción, on the island of Ometepe in Lake Nicaragua, makes floods and tsunamis a potential danger if the volcano were to erupt.

However, shortly afterwards activity at the volcano began to decline, with INETER reporting on 22 March that degassing and seismic activity had fallen to low levels in comparison with the preceding days. On 24 March INETER confirmed a ‘considerable reduction in activity’ but reported continuing ‘anomalous’ levels of seismicity. The current situation is that activity remains low, but the volcano continues to be carefully monitored.

News
El volcán Concepción lanza gases y cenizas sin causar víctimas en NicaraguaEl Norte de Castilla, 8 March 2010
Nicaragua: volcán Concepción presenta columna de cenizas de 20 metros – 123.cl, 10 March 2010
Volcán en Nicaragua lanza toneladas de cenizas y gases, sin causar víctimas – Agencia EFE, 12 March 2010
Volcán nicaragüense vuelve a lanzar columnas de cenizas sin causar víctimasABC, 14 March 2010
Concepción está en plena erupciónLa Prensa, 19 March 2010
Ejército se prepara ante cualquier escenarioEl Nuevo Diario, 20 March 2010
Disminuye actividad del volcán ConcepciónNicaragua Hoy, 22 March 2010
Concepción mantiene sismicidad ‘anómala’La Prensa, 24 March 2010

Information
Global Volcanism Program: Concepción – summary information for Concepción (1404-12=)
Instituto Nicaragüense de Estudios Territoriales – INETER main page
INETER Comunicados Oficiales – INETER volcano bulletins (hopelessly out of date)

The Volcanism Blog

Lowered alert level at Llaima 27 March 2010

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The Chilean state geological service SERNAGEOMIN reports in its latest Llaima bulletin that during 5-22 March 2010 ‘seismic activity around Llaima volcano has in general declined, returning to the levels shown before the earthquake of 27 February’. An overflight on 10 March revealed a low level of fumarolic activity, with occasional small white emissions columns reaching approximately 100 metres above the main crater.

As a result of the low levels of activity, the alert level for Llaima (which was raised on 5 March) has been reduced to Yellow Level 3, but the 4-km radius exclusion zone around the crater is remaining in place, and the volcano will continue to be monitored on a continuous basis.

The full Llaima bulletin covering 5-22 March 2010 is available as a PDF here.

For all our Llaima coverage: Llaima « The Volcanism Blog.

Information
Global Volcanism Program: Llaima – summary information for Llaima (1507-11=)
Oficina Nacional de Emergencia – Chilean government emergencies office
SERNAGEOMIN – Servicio Nacional de Geología y Minería, Chile
Proyecto Observación Visual Volcán Llaima – Llaima Visual Observation Project

The Volcanism Blog

Eyjafjallajökull/Fimmvörduháls at the NASA Earth Observatory 27 March 2010

Posted by admin in activity reports, eruptions, Eyjafjöll, Iceland, NASA Earth Observatory.
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As previewed here (and at Eruptions) yesterday, the NASA Earth Observatory image of the day for 27 March 2010 is the ongoing fissure eruption at Eyjafjallajökull/Fimmvörduháls in south Iceland.

Eruption of Eyjafjallajokull Volcano, Iceland, 24 March 2010 (NASA Earth Observatory)

A commenter here asked about the green colour visible within the fissure and the drainage channel in this image. Robert Simmon of NASA answers that question in the Eruptions comments thread: ‘The green along the margin of the lava flow is an artifact of the satellite sensor. The true-color image is the combination of a 30m/pixel RGB image with a 10m/pixel panchromatic image. Each color pixels covers the same area as 9 panchromatic pixels, so you’ll occasionally get odd colors in high contrast areas’.

Eruption of Eyjafjallajökull Volcano, Iceland – NASA Earth Observatory, 27 March 2010

Information
Global Volcanism Program: Eyjafjöll – summary information for Eyjafjallajökull, which the GVP calls Eyjafjöll (1702-02=)
Eyjafjallajökull eruption March 2010 – summary of events from the University of Iceland’s Nordic Volcanological Center
Photos from Fimmvörðuháls – images and information from the Iceland Meteorological Office

The Volcanism Blog

Eyjafjallajökull update, 26 March 2010 (updated) 26 March 2010

Posted by admin in activity reports, eruptions, Eyjafjöll, Iceland.
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Volcanic eruption at Fimmvorduhals, 24 March 2010 (NASA image, ALI/EO-1)

Above is a labelled detail of an image of the current Eyjafjallajökull (or Fimmvörduháls) eruption in Iceland, captured by the Advanced Land Imager aboard NASA’s EO-1 satellite on 24 March 2010 and reproduced here courtesy of the NASA Earth Observatory. The active fissure can be seen bottom left, with its lava fountains and its plume of gas and ash, with a predominance of water vapour indicated by its light colouring. The smaller plume in the centre is produced not by an additional fissure but by phreatomagmatic activity caused by the lava flow which can be seen flowing north-east from the seat of the eruption encountering an abrupt steepening of its descent (as reported here). This image was sent over by Robert Simmon in advance of its publication at the NASA Earth Observatory site: our grateful thanks to Robert for the preview.

Yesterday ‘increased force’ in the eruption was reported, but today the webcams appear to show diminished activity (although the reduction of ice and snow in the vicinity of the eruption through melting may also be playing a role in reducing the scale of the eruption plumes). A warning has been issued about toxic fumes in the vicinity of the eruption: sulphur, flourine, carbon dioxide and carbon monoxide are being released by the activity. Seismically things appear fairly stable underneath Eyjafjallajökull and Katla and there is little sign of the latter stirring, although prudent preparations are under way locally, just in case. There has been much media speculation about the potential global consequences of a Katla eruption; New Scientist has an oddly-titled but sober assessment, only giving in to temptation and mentioning Laki 1783 at the very end.

Thanks to Steinar Sigurðsson of Icelandic Mountain Guides for sending a link to this report on his site: Eyjafjallajökull volcano erupts in Iceland (23 March 2010). There is also a very useful collection of links relating to the eruption at this Eyjafjallajökull links page.

UPDATE: If this eruption builds a mountain, it will need a name. What should the new mountain be called?

News
Iceland waits for volcanic shoe to dropNew Scientist, 22 March 2010
Two-hundred meter high lava fall in South IcelandIceland Review Online, 24 March 2010
Increased force in South Iceland volcanoIceland Review Online, 25 March 2010
Global cooling: what happens if the Iceland volcano blowsUSA Today, 25 March 2010
South Iceland inhabitants prepare for second eruptionIceland Review Online, 25 March 2010
Toxic fumes at source of Iceland eruptionIceland Review Online, 26 March 2010

Information
Global Volcanism Program: Eyjafjöll – summary information for Eyjafjallajökull, which the GVP calls Eyjafjöll (1702-02=)
Eyjafjallajökull eruption March 2010 – summary of events from the University of Iceland’s Nordic Volcanological Center

The Volcanism Blog

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