Eopleistocene

The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.

Eopleistocene

the lower subdivision of the Anthropogenic system, including the beds of Pleistocene glaciations (through the Mindel glaciation) and the interglacials [see Figures 1 and 2 in ANTHROPOGENIC SYSTEM (PERIOD)]. The name was adopted by the Commission for an International Map of the Quaternary Deposits of Europe in 1932. It was subsequently used as the name of the Lower Anthropogene, corresponding to the Mindel glaciation and the preceding interglacial.

Various Soviet geologists, such as V. I. Gromov and K. V. Nikiforova, consider the Eopleistocene to be the lower subdivision of the Anthropogene from its beginning through the Giinz glaciation.

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References in periodicals archive ?

The river valleys have up to 10 alluvial formations from Eopleistocene to Holocene inclusive.

Rock lithology role at spatial analysis of Russian Plain eastern part climatic skewness

and Przybylski, B.: 2004, Evolution of the Late Neogene and Eopleistocene fluvial system in the Foreland of Sudetes Mountains, SW Poland.

Geodynamics of south-eastern part of the Central European subsidence zone

and Przybylski, B.: 2004, Late Neogene and Eopleistocene evolution of fluvial system in the Foreland of Sudetes Mts., Annales Societatis Geologorum Poloniae, in print.

Cainozoic evolution of lower Silesia, SW Poland: a new interpretation in the light of sub-Cainozoic and sub-Quaternary topography

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