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Lowland glaciers are usually considered the best analogs for
formerly glaciated areas and as such, many Icelandic glaciers have
been intensively investigated with regard to process-orientated
sediment-landform interrelationships. The Myrdalsjokull ice cap
has, thus, served as an excellent "ice-age laboratory."
Furthermore, a substantial effort has been directed
towardunderstanding the interaction between volcanic activity and
glacier response, such as meltwater outbursts (jokulhlaups) and
sudden events of rapidly flowing glacier ice. The book reviews the
following themes related to Myrdalsjokull: glaciology, glacial and
quaternary geology, sedimentology, tephrochronology and eruption
history of Katla, and crustal movements. All authors are involved
in research about the subglacial Katla volcano and Myrdalsjokull.
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