АРИДНЫЕ ГОРЫ

dc.contributor.author	Уфимцев Г.Ф.
dc.date.accessioned	2024-03-09T07:07:16Z
dc.date.available	2024-03-09T07:07:16Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=9213561
dc.identifier.citation	Геоморфология, 2006, , 2, 21-33
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/42931
dc.description.abstract	There are 3 main types of the arid mountains: the desert (extra-arid) mountains, the mountains of the piedmonts, the high-mountains and the arctic mountains. Their development occurs under the eolian activity, saprolitization and desquamation. Within the arid mountains, there are two main morphological types of landscape: - "real" mountains in the active phase of development and "ruin" mountains in the "residual" phase of development. The belts of scours on the slopes combining with the desquamation surfaces are characteristic of the first type; foothills and piedmonts are widespread within the second one.
dc.title	АРИДНЫЕ ГОРЫ
dc.type	Статья
dc.subject.udc	551.4.432:551.585.53(100)

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