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  • Consideration of the structure and morphology of the study area as a whole, as well as that of a small constructional volcanic hill suggests that it evolved in two phases. The principal phase of development involved a period of crustal extension
  • portion of the Mitchell Plain. They display multiple levels and distinct passage morphologies, which, it is argued, illustrate their particular reaction to base-level lowering.
  • The development of medial moraine on the Glacier de Tsidjiore Nouve is related to numerous englacial debris layers of limited dimensions, which are exposed at the glacier surface below the Pigne d'Arolla ice fall. The morphology of the debris layers