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|Collaborative Proposal: Glacier seismicity and its relationship to basal motion (Norway Glacier/CWU)
The PIs propose to locally induce rapid glacier slip, measure it directly at the bed, and study the seismic expression of that slip. This work can be accomplished only at the Svartisen Ice Cap in Norway, where tunnels in subglacial rock provide unusual access to the bed of a thick sliding glacier.
|Digital Object Identifier (DOI)
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