0.71 Mb)
Earthquakes Bárðarbunga - all earthquakesEarthquakes Bárðarbunga earthquakes - 3D video
Earthquakes Bárðarbunga earthquakes - 3D interactive model
GPS map Bárðarbunga GPS displacementsSubsidence Vertical displacement in the Bárðarbunga calderaGas observ. Volcanic gas detectedGas observ. I want to reportGas observ. View public
/volcanoes/about-volcanoes/bardarbunga/the-bardarbungaholuhraun-eruption/
events (download as pdf 0.92 Mb)
Update Bárðarbunga 2015 - February events (download as pdf 1.28 Mb)
Update Bárðarbunga 2015 - March-April-May follow up (see pdf 0.71 Mb)
Earthquakes Bárðarbunga - all earthquakes
Earthquakes Bárðarbunga earthquakes - 3D video
Earthquakes Bárðarbunga earthquakes - 3D interactive model
GPS map
/earthquakes-and-volcanism/articles/nr/2947/
Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009
ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost
operating manage- ment develop- poned-, of land grants ons European tax over- level
costs ment ment comprehen- build- and com- Regional De- heads
1991- 1991- sive- and ings pensation
/media/loftslag/Traffc-maintenance_expenditures.pdf
and explored. The list of earthquakes updates every five minutes. Click this link to run the model:
An interactive 3D model of the earthquakes in Bárðarbunga – preliminary version
However, this is a preliminary version; the model is still being developed. There are some browser issues, e.g. Google Chrome and Firefox run it, IE10 does not; other browsers have yet to be tested. In some instances
/earthquakes-and-volcanism/articles/nr/2971
and explored. The list of earthquakes updates every five minutes. Click this link to run the model:
An interactive 3D model of the earthquakes in Bárðarbunga – preliminary version
However, this is a preliminary version; the model is still being developed. There are some browser issues, e.g. Google Chrome and Firefox run it, IE10 does not; other browsers have yet to be tested. In some instances
/earthquakes-and-volcanism/articles/nr/2971/
the average of the (wind speed) distribu-
tion is given by
m = AG(1+1=k) ; (2)
with gamma function, G, defined as usual. Wind power density, a measure of the energy flux
through an area perpendicular to the direction of motion, varies not only with the cube of wind
15
Figure 2. Annual modelled distributions (dashed lines) and corresponding Weibull fits
(solid lines) of wind speed at 50 mAGL, for two
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
in thickness
within Geldingadalur rather than spreading out. Ongoing work on processing
geochemical and gas data is being done, and the graphs will be updated as soon
as it is completed.3D model of the
eruption sitesThe Icelandic Institute of Natural History
operates an aerial photography studio where geological mapping is carried out
using aerial photographs to create three-dimensional
/about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir
/lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13
April 2009.
[2] WTO, World Tourism Organization (2008): “Climate Change and Tourism -
Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain.
Available at:
http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7
March 2010.
[3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for
sustainable
/media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf
September
Ari Tryggvason and others
Relative locations in 3D velocity models
Ásta Rut Hjartardóttir and others
The Kerlingar fault, north east Iceland, a Holocene normal fault east of the divergent plate boundary , Extended abstract
Björn Lund and others
How may glacial rebound influence the seismic activity in Iceland?
Bryndís Brandsdóttir
/earthquakes-and-volcanism/conferences/jsr-2009/featured/