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  • Observations of sorted patterned ground features, High Valley/Tangle Lakes region, Central Alaska, U.S.A. in Periglacial processes and landforms.
  • The implications of investigative design for the study of fluvial sediment transfer in arctic and subarctic regions in Periglacial processes and landforms.
  • Analysis of the fluvial deposits occurring in the Weichselian basin fills in the Twente region contributes valuable information to the interpretation of last Glacial paleoenvironments. Although quantification of paleohydrologic data is difficult
  • zone (Seppälä 1988). This distinction is thought to be necessary because research activities in the high Arctic regions are continuously increasing and there is confusion if all frozen peat mounds are described as palsas.