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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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Published in: | Revista Mexicana de Ciencias Geológicas |
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Main Authors: | , |
Format: | Artigo |
Language: | Inglês |
Published: |
Universidad Nacional Autónoma de México
2004
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Subjects: | |
Online Access: | https://www.redalyc.org/articulo.oa?id=57221111 |
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