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Regional scale Finite Element modelling of the dynamic movements
following episodes of volcanic activity will help planning the supply of temporal
instruments from other projects and/or future network configurations. This work will be started
on the basis of existing deformation data from GPS and ground observations
of German geodetic groups during and
after the Krafla fissure eruptions in North Iceland. This work will be
linked to, and gain from, the future permanent recordings of the HOTSPOT
Observatory.
Margret Asgeirsdottir
1999-09-07