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The Bryansk fossil soil of the extraglacial zone of the Valday glaciation as an indicator of landscape and soil forming processes in the center of the Russian Plain

The morphologic-analytical features of the Bryansk fossil soil classified as Umbric Gley Soilformed in moraine loams and overlain by Upper Pleistocene moraine of the Valday (Würmian) glaciationare described. This paleosol, formed during the Dunaevo Interstadial of the upper Pleistocene andcorrespond...

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Bibliographic Details
Published in:Revista Mexicana de Ciencias Geológicas
Main Authors: Alexey V. Rusakov, Mariya A. Korkka
Format: Artigo
Language:Inglês
Published: Universidad Nacional Autónoma de México 2004
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Online Access:https://www.redalyc.org/articulo.oa?id=57221111
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