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  • Relict talus-foot rock glaciers at Øyberget, Upper Ottadalen, Southern Norway : Schmidt hammer exposure ages and palaeoenvironmental implications
  • Three relict talus-foot rock glaciers at Øyberget, upper Ottadalen, were dated using high-precision Schmidt hammer exposure-age dating (SHD). A SHD calibration curve was constructed for the local banded gneiss using 2 control points : 1) fresh
  • 2013
  • to be maintained by a standing man hiking in the Łysogóry Range on a frosty and windy winter day. Summer sports clothing (Iclp = 1.00-1.50 clo) seems to offer sufficient protection for a standing man at the foot or on the slopes of the Łysogóry Range during a warm
  • 2013
  • a.s.l. as lower permafrost limit. Palaeo permafrost was identified at 3,400-3,500 m a.s.l. approximately on the foot of the southern slope of the Maipo Volcano. At present, the zone, still in a paraglacial state, is characterized by intense cryodynamics
  • 2013
  • of actively accumulating features. A more robust set of criteria, derived from common characteristics of actively accumulating ramparts, are proposed that assists in discriminating relict and active pronival ramparts from other discrete bedrock cliff-foot
  • 2013