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  • Cirque glaciaire ; Europe ; Europe centrale ; Glaciation ; Limite d'enneigement ; Montagne ; Pléistocène ; Pologne ; Quaternaire ; Sudety ; Tchèque, république ; Topographie ; Vallée glaciaire
  • Central Europe ; Cirque ; Czech Republic ; Europe ; Glacial valley ; Glaciation ; Mountain ; Pleistocene ; Poland ; Quaternary ; Snow line ; Sudety ; Topography
  • The pattern and magnitude of the Pleistocene glaciation in the Sudetes is clearly controlled by the pre-existing, preglacial topography. The simultaneous occurrence of 3 factors is considered necessary for a mountain glaciation to develop
  • The aim of this paper is to review existing information about weathering mantles in the Sudetes and the Sudetic Foreland and to evaluate their usefulness in the evolutionary approach to the origin of the Sudetic topography. The observed diversity
  • primarily reflects long-term differences in tectonic and geomorphic stability of these 2 areas, accentuated through time. Moreover, weathering mantles are used to strengthen the argument for etched origin of many facets of Sudetic topography.
  • The Sudetes Montains are characterised by a residual tectonic topography, the typical landform being mature fault-generated range fronts originated during the Late Tertiary. The general pattern of neotectonic movement in this area can be inferred
  • Granite topography of the Veladero massif, south Mexico, is a heavily dissected all-slopes type of relief. Rock slopes and tor-like residuals occur near the crests, whereas exposures within middle and lower slopes show deeply disintegrated granite