
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.
ПЛЕЙСТОЦЕНОВЫЙ ПЕРИГЛЯЦИАЛ, СКЛОНОВЫЕ ПРОЦЕССЫ, ДЕЛЛИ
ПЛЕЙСТОЦЕНОВЫЙ ПЕРИГЛЯЦИАЛ, СКЛОНОВЫЕ ПРОЦЕССЫ, ДЕЛЛИ
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