ОСОБЕННОСТИ СТРОЕНИЯ РЕЛЬЕФА СКАЛЬНОГО ЛОЖА ГОРНЫХ И ПОЛУГОРНЫХ ДОЛИН

dc.contributor.authorСысоева С.М.
dc.contributor.authorВиноградова О.В.
dc.date.accessioned2022-05-08T02:20:21Z
dc.date.available2022-05-08T02:20:21Z
dc.date.issued2004
dc.description.abstractA 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.identifierhttps://www.elibrary.ru/item.asp?id=17345354
dc.identifier.citationГеоморфология, 2004, , 4, 48-54
dc.identifier.issn0435-4281
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/37455
dc.subject.udc551.435.11(235.3)
dc.titleОСОБЕННОСТИ СТРОЕНИЯ РЕЛЬЕФА СКАЛЬНОГО ЛОЖА ГОРНЫХ И ПОЛУГОРНЫХ ДОЛИН
dc.typeСтатья

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