Alfonz Gajdoš

Glaciálne formy georeliéfu na svahoch Prašivej v Nízkych Tatrách

Glaciation on south slopes of the Prašivá massif in the Low Tatras Mountains

Abstract:

The article is focused on problematic glaciation on south slopes of the Prašivá massif in the Low Tatras Mountains.We analyse possition of erosion and accumulation form of georelief
(glacier kettle and moraine wall originated from meridian würm glacial stage). The author takes information from geological maps of the posttertiary period in Low Tatras Mountains, from works published after 1970 and from own terain survey in the Husárka valley underneath the Mount Košarisko located on the south slope of Prašivá massif.

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