Реконструкция масштабов и морфологических особенностей плейстоценовых оледенений на Северо-Востоке России

Based on the currently available data, it has been established that the earliest glaciations occurred in the Late Eopleistocene and at the end of the Early Neopleistocene. They had local distribution in the most uplifted parts of the Chersky Range. Their traces are presented in the form of moraines ... View More