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О происхождении деллей на территории Закамья Республики Татарстан

О происхождении деллей на территории Закамья Республики Татарстан

Abstract

Дается морфологическая характеристика деллей форм мелкорытвинного расчленения склонов, образовавшихся в плейстоценовой перигляциальной зоне востока Русской равнины в эпоху ее последнего, осташковского, оледенения.

The morphological characteristics of the dales (forms of slope dissection) formed in Pleistocene periglacial zone in the eastern part of the Russian plain during the Ostashkov Ice Age are given.

Keywords

ПЛЕЙСТОЦЕНОВЫЙ ПЕРИГЛЯЦИАЛ, СКЛОНОВЫЕ ПРОЦЕССЫ, ДЕЛЛИ

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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
0
Average
Average
Average