to the recent
high seismic activity and subsurface magma flow to the northeast.
In the surveillance flight yesterday a shallow, wide depression was observed on the
surface of Dyngujökull, 10 km from the glacier edge. Another depression
6 km from
the Dyngjujökull ice edge, which has been monitored over the last few days has
deepened and is now
35 m deep.
o It is likely that these depressions
/media/jar/Factsheet-Bardarbunga-140906.pdf