Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9198
AuthorsOlivieri, M.* 
Spada, G.* 
TitleIce melting and earthquake suppression in Greenland
Issue Date2015
Series/Report no./9 (2015)
DOI10.1016/j.polar.2014.09.004
URIhttp://hdl.handle.net/2122/9198
KeywordsGreenland
Earthquakes
Ice sheet melting
Subject Classification02. Cryosphere::02.02. Glaciers::02.02.05. Ice dynamics 
AbstractIt has been suggested that the Greenland ice sheet is the cause of earthquake suppression in the region. With few exceptions, the observed seismicity extends only along the continental margins of Greenland, which almost coincide with the ice sheet margin. This pattern has been put forward as further validation of the earthquake suppression hypothesis. In this review, new evidence in terms of ice melting, post-glacial rebound and earthquake occurrence is gathered and discussed to re-evaluate the connection between ice mass unloading and earthquake suppression. In Greenland, the spatiotemporal distribution of earthquakes indicates that seismicity is mainly con- fined to regions where the thick layer of ice is absent and where significant ice melting is presently occurring. A clear correlation between seismic activity and ice melting in Greenland is not found. However, earthquake locations and corresponding depth distributions suggest two distinct governing mechanisms: post-glacial rebound promotes moderate-size crustal earthquakes at Greenland’s regional scale, while current ice melting promotes shallow low magnitude seismicity locally
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