of volcano-
tectonic structures are sets of parallel, northerly striking transcurrent faults that generate the largest
earthquakes in this zone, up to M 6.5. Their surface expressions are en echelon fracture arrays and
push-up structures. The sense of displacement is right-lateral. The distance between them varies from
0.5 to 5 km, and together they form a bookshelf-type fault system taking up the left
/media/norsem/norsem_palli.pdf
) noted that Iceland had a maritime
climate that was much milder than its position on the globe might suggest. In
data from 1981–2010, Iceland annual average temperatures ranged from 6°C at the
south coast to 3°C at the north coast, with a substantially colder highland
interior. In comparison with the latitudinal average for the same period, the
coastal temperatures in Iceland are 8–10°C warmer
/climatology/iceland/climate-report
) noted that Iceland had a maritime
climate that was much milder than its position on the globe might suggest. In
data from 1981–2010, Iceland annual average temperatures ranged from 6°C at the
south coast to 3°C at the north coast, with a substantially colder highland
interior. In comparison with the latitudinal average for the same period, the
coastal temperatures in Iceland are 8–10°C warmer
/climatology/iceland/climate-report/
this
perspective, states do things differently nowadays
because they operate in different network
formations and use other instruments. However, in
this perspective the state is still the engine that keeps
the motor running. In contrast, society-centered
perspectives even consider the possibility of
‘governance without government’ (Rhodes 1996).
A particular type of governance concept that has
been thriving
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
Type: Subglacial volcano with caldera
Summit ice cover: Yes
Dominant type of activity: Basaltic explosive, phreatomagmatic
Magma type: Basalt dominant
Known precursors: No information
Expected precursors: Significant increase in seismic activity
Monitoring level: High
Current seismicity: Seismic swarms from 16 August 2014. See http://vedur.is for live
information
Eruption
/media/jar/Bardarbunga_kafli20140825.pdf
Reykjavík 16. janúar 2010.
Til: Veðurstofu Íslands.
Frá: Landhelgisgæslu Íslands.
Efni: Hafískönnun 16. janúar 2010.
Laugardaginn 16. janúar 2010 fór þyrla landhelgisgæslunar TF-EIR í gæslu og ískönnunarflug. Var flogið
norður Húnaflóann og fyrir vestfirðina.
Einn stakur ísjaki sást í Húnaflóanum á stað : 66°12,7‘N – 21°16,3‘V
Komið var að ísröndinni út af Húnaflóa og henni fylgt til vesturs um
/media/hafis/skyrslur_lhg/Isskyrsla_20100116_rett.pdf
conditions
An interactive weather map shows weather observations at any station in the country.
Installation
Get the weather app at Google Play Store or Apple App Store. Type VEDUR or vedur to find the app and install. Select language under Settings (Stillingar), shown in the video below.
Video instructions
A video shows all the features of the weather app for those who want to familiarise
/about-imo/news/nr/3224
the volcano. Question: Should an eruption occur, where from the glacier can
the jökulhlaup be expected?Answer: It depends on the
location and type of the eruption. Three types of glacial outbursts can be
thought about:Floods resulting from an eruption
in the caldera, where the ice is up to 500 m thick. Large eruptions can melt of order 100,000 m3/s.
Jökulhlaups can be expected from Virkisjökull
/volcanoes/about-volcanoes/oraefajokull/q-a/