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Ultramorphoscopic analysis offers one way of gaining an insight into temporal and spatial changes that have taken place in the environment. The underlying basis here is a system of classified features; processes of physical, chemical and biological weathering; and processes of transport through different environments. It is the aim of this article to present the use of morphoscopic SEM studies of podsolic soils from different parts of central and northern Europe in reconstructing the way lithoand pedogenetic conditions evolved in the Late Pleistocene and Holocene. By drawing on the research carried out, it has been possible to point to certain indicative morphoscopic features of quartz grains that are characteristic for defined morphogenic environments.

The use of sem morphoscopy in researching the litho-pedogenetic environments evolution of Late Pleistocene and Holocene