Abstract
The article presents morphological classification of debris flow basins for folded Carpathian Mountains on the basis of existing common classifications and features of geological and geomorphological structure of the examined region. It was substantiated to using the term "debris flow body", which means the accumulated fragmental product of debris flow origin. The morphogenetic types of debris flow bodies were highlighted. The classification of debris flows for folded Carpathian Mountains by their solid phase supply was also elaborated.
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