Ríðum, ríðum, rekum yfir sandinn,
rennur sól á bak við Arnarfell.
Hér á reiki’ er margur óhreinn andinn
úr því fer að skyggja á jökulsvell.
This is one of the most famous Icelandic folk songs, talking about people riding over the highland desert, on the Sprengisandur track, hurrying on horseback over the barren land between the majestic glacier volcanoes, thinking about ghosts haunting the wind-blown valleys between Hofsjökull and Vatnajökull.
This is Hofsjökull glacier volcano. But they will also be traveling past Bárdarbunga volcano. Without being as well-known and popular with the media as her colleagues Katla and Hekla, Bardarbunga is a volcano which deserves remembering.
Bárdarbunga, a big volcanic edifice and central volcano located under Vatnajökull in Iceland, has been showing unrest for some time now. There was esp. the glacier run (jökulhlaup) from June 2011 into the reservoir Hágöngulón in the highlands of Iceland. But also lately, growing unrest showed on the tremor charts of IMO:
Under the five big ice caps which together cover about 10 % Iceland’s surface, there are located 9 or 10 central volcanoes incl. parts of their fissure systems. Under Vatnajökull alone, there are 2 twin systems of basaltic and rhyolitic central volcanoes, i.e. Grímsvötn-Gjálp and Bárdarbunga – Hamarinn/Loki-Fögrufjöll, Kverkfjöll in the north, all of these part of the EVZ (Eastern Volcanic Zone of Iceland), and two separate active central volcanoes, Esjufjöll and Öraefajökull, forming a separate belt in the east. (Thordarson, 2007)
Bárdarbunga central volcano, proudly presenting a 80 km2 caldera with a depth of 700 m, and reaching heights of 2100 m at its summit, is placed in the northwestern part of Vatnajökull ice cap, north of Grímsvötn.
Of these volcanic systems, Grímsvötn is by far the most productive with 480 eruptions in 6.500 years, whereas Bárdarbunga prehistoric eruption frequency (which means in Iceland till 1.000 BP) reaches 330 eruptions during the same period of time and an average of 5 per century. On the other hand, tephra layers from Bárdarbunga are dispersed more widely, which indicates „more voluminous and/or longer lasting eruptions than these of Grímsvötn“. Additionally, there were 135 tephra layers which could be identified with Grímsvötn, 87 originating from Bárdarbunga and only 17 from Kverkfjöll since Icelandic settlement started in the 9th century. This gives Bárdarbunga the place of the 2nd or third most active volcanic system in Iceland in historic and prehistoric times – rivaling Hekla. (Larsen, 2011). But probably there were much more eruptions, mostly very small ones which couldn’t break the glacier surface. See also GVP: http://www.volcano.si.edu/world/volcano.cfm?vnum=1703-03=&volpage=erupt
But Bárdarbunga also has the longest or perhaps – if Askja is competitive enough – the second longest fissure system of Iceland (around 190 km), extending to the south into the Landmannalaugar region (Veiðivötn, Vatnaöldur) and also some 50 km in northeastern direction from her outlet glacier Dyngjujökull. It produced not only one of the most important flood eruption events in historic time (Veiðivötn in 1480), but also an enormous lava field, the so-called Þjórsárhraun (2130 km3) 8.500 years ago.
There has now been some earthquakes, one of them magn. 3.3. Like many other calderas, she shows unrest from time to time, which may or may not mean more. This is anyways a volcano which deserves some attention.
See also Carl’s post about Hamarinn: https://volcanocafe.wordpress.com/2012/01/25/hamarinn-volcano-burns-night/
- Volcanism in Iceland, by Th. Thordarson, G. Larsen (2007)
- Basaltic Tephra Layers reveal the Eruption History of the Icelandic subglacial Volcanoes, Grimvötn, Bardarbunga and Kverkfjöll during the last 7000 Years, by B. A. Oladottir, G. Larsen, etal. (2011)
PS: Disclaimer – I am just a layman interested in geology.
264 thoughts on “Bárdarbunga calling”
Bárðarbunga straining to live up to the expectations: http://hraun.vedur.is/ja/oroi/dyn.gif 😉
Yup! I am still watching. I must admit to a wicked desire to see this volcano erupt tomorrow. 😀
I believe that Bardarbunga could have an eruption sometime within the next months or even weeks. Still its an unconventional scenario, since the volcano has been long dormant.
An eruption would most likely be similar to that of Eyjafjallajokull, around VEI4. But probably with a larger intensity at the beginning (like Grimsvotn) and with a large glacial flood. Still, this would be something on the scale that Iceland ocasionally has.
Or this can be linked to a hotspot entry of magma.
Mr Irpsit, what does the Bardarbunga name translate to in English please?
Just because I have always loved this song……..It takes me back to my mis-spent youth. 😀
Had a good friend who could sing like Johnny.Problem was he wasn’t imitating
he really could sing like him. He was a Norwegian-American from North Dakota..
Johnny Mathis and Nat King Cole.. they broke the mold on both…
Hi tgmccoy 😀 I am glad to see you returned from the nether regions of Walmart safely :D. You know, all these talent shows and X factor carp and not a one can REALLY sing without electronic back ups. I am sure it isn’t just my age that makes me find singers today lack that deep, vibrant yet silky tones.
OMG! It has begun! http://i48.tinypic.com/2a4z5a8.jpg
Oh my heart just made a big jump – add one blob, somebody!
My Goodness… Right on time too. Are these quakes Magmatic or tectonic? If tectonic then as the plates move We may get shoved over to the USA… I could drive over and see Lurking 😀
Hey, those are only the manually revised ones, not the automatically detected earthquakes, since noone survived, this map is wrong by default 😉
New post is up: Hurray, it’s DOOMSDAY!
And yeah. The double comment is not coincidence.
New DOOMSDAY post is up!!!
#Pacaya volcano, #Guatemala. Return of eruptions in past 48 hours has created a new crater.