of this type may represent a serious risk if they occur in tourist spots such as the Askja region.
We present observations of the July 21st, 2014 event as recorded by the national infrasonic arrays
network installed in the country within the FUTUREVOLC European project. Infrasound released by
the event was recorded at a distance of 210 km from Askja volcano.
We performed 2D FDTD modeling
/media/norsem/norsem_giulia.pdf
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
Fjölbrautaskólanum við Ármúla
Kristín S. Vogfjörð, Veðurstofu Íslands
VÍ 2009-012
ISSN 1670-8261
Skýrsla
+354 522 60 00
+354 522 60 06
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 9
150 Reykjavík
5
Project no. 036935
Project acronym: SAFER
Project title: Seismic eArly warning For EuRope
Instrument : Specific Targeted Research Project
Thematic Priority: Sustainable development
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
northnorthwest of Straumsnesviti and about 60 nm northwest of Barði. Easterly and northeasterly winds were dominant in the Greenland Strait and the sea ice was far off shore the whole month. No dispatches from ships were received from ships and the Coast Guard did not go on an exploration flight
/sea-ice/monthly/2009/nr/2324
during the month. IMO issued information regarding sea ice around mid-month, based on satellite images. The information showed the sea ice was closest to shore about 60 nm northwest of Barði. Easterly winds were predominant in the Greenland Strait
/sea-ice/monthly/2009/nr/2327