Polish and NW Ukrainian loess covers are situated along the northern margin of the central
part of the European loess belt. Because of their intermediate geographic position, they form …

The study focuses on the loess–palaeosol sequence at Roxolany, exposed in the cliffs on
the left bank of the Dniester Liman in the Black Sea Lowland. The sequence is one of the …

Loess sediments have proved to be the most significant palaeoclimatic and
palaeoenvironmental archives on land and thus present an important part of the Earth's …

Loess areas used for agriculture are susceptible to soil erosion. The intensive process of soil
erosion in Polish loess areas began with the onset of the Neolithic and has continued …

Closed depressions are reported in loess landscapes in various parts of Europe. The
anthropogenic and natural origin of closed depressions is highly debated in literature …

In the well-known settlement micro-region of the Małopolska Upland-known for extensive
studies into the Neolithic agricultural anthropopressure-the authors have re-examined three …

Loess formations in Poland display a close relationship with cooling and warming trends of
the Northern Hemisphere during the Pleistocene. Loess sequences sensitively record …

The article presents the results of micromorphological studies of selected Neopleistocene
loess-palaeosol sequences. Broader studies of thin sections are presented for the Polanów …

Cliff‐related talus accumulations are often highly affected by post‐depositional processes,
and the sedimentological characteristics are poorly documented, especially in arid settings …

Abstract The Kraków Spadzista open-air site, situated in the loess belt in southern Poland,
belongs to the best-known Gravettian sites of Europe. Many years of archaeological studies …