CRUSTAL DEFORMATION
Measurements of the movement of the earth's crust provide data on the
amount and temporal distribution of deformation that takes place, preceding,
during and after the occurrences of earthquakes and volcanic eruptions.
These data can be extracted from global positioning satellite, radar interferometry
and repeated gravity observations. Research in these areas is being conducted
under the aegis of the research groups Crustal
Deformation and Fault Mechanics and Radar
Interferometry and the faculty members Paul
Segall and Howard Zebker.
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