DEBRIS FLOW AT LOG POD MANGARTOM
Abstract
This paper analyzes the Stože landslide from the aspect of debris flows described in world literature. The principal characteristics of the debris flow are compared with those of investigated phenomena around the world. The occurrence of debris flow is very rare in Slovenia, but quite frequent in mountainous areas all over the world. For this reason the typical characteristics of debris flow are well known. This article examines the typical characteristics of debris flows and compares them to the one in Log pod Mangartom. Finally, the particularities of the Stože debris flow are exposed. A comparison shows that the Stože debris flow has all the typical characteristics of debris flows, as it displays certain particularities, such as two phases of the course of events.
References
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