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• 1. norsem_korja

  fault zone in the Kuusamo area, the gradient seems to be associated with a zone of increased seismicity. In these areas, the crustal thickness gradients are optimally oriented for reactivation. Because the spatial distribution of the registered earthquakes exhibits little to no correlation with the an existing ellipsoidal rebound model or Glacial Isostatic Adjustment (GIA /media/norsem/norsem_korja.pdf

• 2. The Icelandic glaciers weighed from space

  not intended to monitor changes of “smaller” glaciers such as the glaciers in Iceland. Many factors have to be taken into consideration and several corrections applied in order to measure mass changes of small glaciers, including the effect of vertical crustal movements induced by changes in glacier loads over the last century on the gravity field (so-called glacial isostatic adjustment or GIA /about-imo/news/the-icelandic-glaciers-weighed-from-space