ОСОБЕННОСТИ СТРОЕНИЯ РЕЛЬЕФА СКАЛЬНОГО ЛОЖА ГОРНЫХ И ПОЛУГОРНЫХ ДОЛИН

dc.contributor.author	Сысоева С.М.
dc.contributor.author	Виноградова О.В.
dc.date.accessioned	2022-05-08T02:20:21Z
dc.date.available	2022-05-08T02:20:21Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=17345354
dc.identifier.citation	Геоморфология, 2004, , 4, 48-54
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/37455
dc.description.abstract	A particular class of channel landforms is described. It is represented by sculptured-erosion forms, created by channel flow cutting into bedrock of mountain and semi-mountain rivers. The main types of this landform class, their changes along the valley, and their dependence on channel type and lithology are considered.
dc.title	ОСОБЕННОСТИ СТРОЕНИЯ РЕЛЬЕФА СКАЛЬНОГО ЛОЖА ГОРНЫХ И ПОЛУГОРНЫХ ДОЛИН
dc.type	Статья
dc.subject.udc	551.435.11(235.3)

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