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 Submarine permafrost degradation rates may be determined by a number of interacting processes, including rates of sea level rise and coastal erosion, sea bottom temperature and salinity regimes,… Continue Reading
Non-consolidated sections of the arctic coastline are generally rich in ground ice and highly dynamic due to the combined effects of thermal abrasion and ero-sion. Subsidence following thaw may… Continue Reading
The causes for the formation of large igneous provinces and hotspot trails are still a matter of considerable dispute. Seismic tomography and other studies suggest that hot mantle material rising… Continue Reading