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The Sudetes are mountains of outstanding geomorphic diversity. Reasons reside in lithological and structural variability of bedrock and protracted history of landscape evolution spanning at least the entire Cenozoic. Over this time span, global changes have exerted a key control on the geomorphic evolution of the Sudetes. Late Cenozoic mountain building in the Alpine-Carpathian region induced differential uplift of the Sudetes and radically changed its geomorphic environment, from one typified by a landscape of low relief to one of increasing relief energy and accelerated erosion. Environmental changes were equally profound but their geomorphic effect is less obvious, except for the widespread presence of periglacial landforms of Pleistocene age and localized occurrence of glacial cirques and moraines in the Karkonosze Mts. At the same time, rock control on the location and shape of individual landforms is evident and large tracts of the Sudetes may be described as having structural morphology. Therefore, unequivocal recognition of relief generations in the Sudetes is problematic.

Geomorphic diversity of the Sudetes - efects of structure and global change superimposed