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  • The case for a stable East Antarctic Ice Sheet: the background
  • The case for a stable East Antarctic Ice Sheet
  • the case for the stability of the East Antarctic Ice Sheet and includes new work on terrestrial geomorphology and geology, marine cores and ice-sheet modelling.
  • This paper aims to illustrate the implications of one particular case study, in the Swiss Alps, for the understanding of the relationship between river channel form and process, and to raise some of the methodological issues associated with small
  • . Care must be taken, however, in deriving denudation rates from the crustal cooling histories documented by thermochronologic techniques, especially in rapidly eroding terrains, since, in such cases, apparent denudation rates derived from