Volcanic rift-zones and flank instability : an evaluation of ground deformation monitoring techniques
Collapse is part of the growth cycle of volcanoes with active rift-zones. As the volcano develops and grows disequilibrium between the strength of the edifice and the applied stresses, produce instability within the edifice which can potentially lead to catastrophic lateral collapse. The intra-erupt...
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University of Gloucestershire
1999
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.302191 |