Vergleichende Periglazialmorphologie im Winterregengebiet der Atacama

Abstract

The periglacial processes in the winter rainfall area in the High Andes of Chile between Llullaillaco 24°43'S, and Mt. Las Tetas 30°09'S and resulting periglacial phenomena are, presented here. The landforming processes reflect the extremely arid recent and present climate. The range of periglacial landforms, the vertical distribution and association of which is described here, results from the interactions of climate and bedrocks. The upper periglacial limits are the highest of the world. Due to the extreme aridity, glaciers to the north of 26°30'S and rock glaciers to the north of 27°00'S cannot form today. Therefore, their absence is not due to insufficiently low temperatures, but to lack of humidity.