experiments for evaluating the effectiveness of avalanche defence structures in Iceland. Main results and future programme (pdf 0,8 Mb) (Í: Proceedings of the International Seminar on Snow and Avalanches Test Sites, Grenoble, France, 22−23 November 2002, F. Naaim-Bouvet, ed., s. 99−109, Grenoble, Cemagref, 2003, author T. Jóhannesson) [abstract] (html)
Stálgrindur eða snjóflóðanet? Val á tegund
/avalanches/imo/protective/
at the plate boundary, leading to volcanic activity and earthquakes. The
geological units are shown on the map in Figure 1. The Western Volcanic Zone (WVZ)
encompasses the part of the rift which enters land at the western tip of Reykjanes Peninsula
(RP), runs east along the peninsula to the Hengill region, where it turns northward. East off the
Hengill region the rifting shifts approximately 90/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
meteorological services for large areas of the North Atlantic and Green-
land. It is the second largest aviation service region in the world. Over the course of a decade IMO was modernized
and sta?ed to meet the highest international requirements. The Icelandic public and economic sectors, in particular
the fisheries, transportation and agriculture, benefitted hugely from this development making
/media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
A (A1, A2, A3). ........................................................................................... 89
Figure B.2. Rake distribution for mapped faults/clusters in box B, Fagradalsfjall-W. ...... 90
Figure B.3. Rake distribution for mapped faults/clusters in box C, Fagdaralsfjall-E. ....... 90
Figure B.4. Rake distribution for mapped faults/clusters in box D, Kleifarvatn
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf