10:00 - from geoscientist on duty
About 80 earthquakes have been located in the Bárðarbunga area past 24 hours - similar amount as the 24 hours before. Four earthquakes were over M4.0:
28 Oct. 09:37 M4.6
28 Oct. 13:01 M4.6
29 Oct. 02:29 M4.6
29 Oct. 05:23 M4.8
Earthquakes over M3.0 were more than 10 and activity in the northern part of the dike is similar as last days. Visibility is good
/earthquakes-and-volcanism/articles/nr/3011
hours.
Notes from the meeting of the Scientific Advisory Board (0.4 Mb)
29 October 2010 10:00 - from geoscientist on duty
About 80 earthquakes have been located in the Bárðarbunga area past 24 hours - similar
amount as the 24 hours before. Four earthquakes were over M4.0:
28 Oct. 09:37 M4.6
28 Oct. 13:01 M4.6
29 Oct. 02:29 M4.6
29 Oct. 05:23 M4.8
Earthquakes over M3.0 were more than 10
/media/jar/Bardarbunga-2014_October-events.pdf
10:00 - from geoscientist on duty
About 80 earthquakes have been located in the Bárðarbunga area past 24 hours - similar amount as the 24 hours before. Four earthquakes were over M4.0:
28 Oct. 09:37 M4.6
28 Oct. 13:01 M4.6
29 Oct. 02:29 M4.6
29 Oct. 05:23 M4.8
Earthquakes over M3.0 were more than 10 and activity in the northern part of the dike is similar as last days. Visibility is good
/earthquakes-and-volcanism/articles/nr/3011/
was therefore formed
by ice lifting and deformation induced by subglacial water pressures higher than ice
overburden pressure.
The discharge data and the derived size of the subglacial flood path, as indicated
by the volume of water stored subglacially, indicates a development towards more
efficient subglacial flow over the course of the jökulhlaup. Thus, a discharge in the
iii
range 80–90 m3 s 1
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf