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released before from the rims of Askja, although people have not noticed them.
Further rockslides in Askja should, therefore, be expected within the next years, decades or centuries. Consequently, travel near the lake is associated with a certain risk. A person by the lake that notices a landslide should move immediately up the hill and away from the lake. It takes a tsunami wave about 1–2/about-imo/news/nr/2930
; the jam shows up in pink along the river channel. Ice extends about 2 km south of the bridge, as well as reaching over 12 km northwards. Yet another satellite image was received 11 Feb 2015 which shows the northern part of the ice surge.
Ice on the move
Running water carries ice fragments slowly down river. Photo: Bragi Benediktsson, Grímsstaðir.
Lonely guard
Water level
/about-imo/news/nr/3062
measured. The uplift is most likely due to pressure at
the root of the volcano caused by magma intrusion which has been modeled at
around 2 km depth. The uplift is is rapid when compared to other similar
volcanos around the world. An increase in earthquake activity has however not
been detected. A subsidence for the past decades in Askja possibly explains the
low seismicity in addition to partly
/about-imo/news/status-of-unrest-in-askja
conference
10.9.2010
The final conference of the CES project "Future Climate and Renewable Energy - Impacts, Risks and Adaptation" was held in Oslo from 31 May to 2 June. The conference was organised around five themes:
Past and present changes in climate
/about-imo/news/nr/1983