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
monthly bulletin was that of April 2015.
Apart from the destructive earthquake in Italy and the nuclear explosion in the DPRK, the most
significant seismic events recorded by the seismic service at GEUS in the recent period, are a sequence
of earthquakes in the Disko Bay area in West Greenland. Since the beginning of the sequence on April
5th 2016, 95 earthquakes have been
/media/norsem/norsem_voss.pdf
of Kópasker. The earthquake was felt in Svarfaðardalur, around 90 km from
the epicenter. It was followed by an aftershock sequence including a
magnitude 2.9 earthquake. This new swarm occurred about 60 km
south-east of the Grímsey swarm and is also on the Grímsey
Oblique Rift zone (GOR). The M3.6 earthquake in Öxarfjörður had
left-lateral strike slip focal mechanism while the ~ M5 earthquakes close
/about-imo/news/seismic-swarm-east-of-grimsey-on-the-decline