ПРИРОДНО-АНТРОПОГЕННЫЕ ЭКЗОДИНАМИЧЕСКИЕ ПРОЦЕССЫ В РЕГИОНАЛЬНЫХ ГЕОМОРФОСИСТЕМАХ ВОСТОЧНОЙ ГЕРМАНИИ. СТАТЬЯ 1. РЕГИОНАЛЬНЫЙ МОРФОЛОГИЧЕСКИЙ АНАЛИЗ

dc.contributor.author	Макунина Г.С.
dc.date.accessioned	2024-04-05T23:52:46Z
dc.date.available	2024-04-05T23:52:46Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=9433375
dc.identifier.citation	Геоморфология, 2006, , 4, 63-69
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/43361
dc.description.abstract	The hierarchy of the morphological structure of the territory under investigation can be represented at three levels. Mega- and mezomorphosystems are distinguished by dominant and subdominant types of the elementary regional morphosystems (ERMS). ERMS are considered in our study as soil - geomorphological component of undisturbed (quasi-natural) landscape. Similar set of exogenic processes and equal intensity of each process taking place in ERMS determine it as initial object for evaluating human-induced destructive disturbances of the morphostructures' surface. Mega- and mezomorphosystems are differentiated with several types of antropogenic loads.
dc.title	ПРИРОДНО-АНТРОПОГЕННЫЕ ЭКЗОДИНАМИЧЕСКИЕ ПРОЦЕССЫ В РЕГИОНАЛЬНЫХ ГЕОМОРФОСИСТЕМАХ ВОСТОЧНОЙ ГЕРМАНИИ. СТАТЬЯ 1. РЕГИОНАЛЬНЫЙ МОРФОЛОГИЧЕСКИЙ АНАЛИЗ
dc.type	Статья

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