Basic surface features of the Łask Interfluve near Zduńska Wola originated during the Wartanian ice-sheet areal deglaciation. The ice-sheet waning resulted in formation of groups of crevasse landforms such as kame plateaux, kame hillocks, kame terraces and melt-out depressions. The post-Wartanian morphogenesis increased diversity of the relief by rejuvenation of most of buried valleys, by cutting new valleys and raising the interfluve surface with aeolian sheets and dunes. Sand and silt were deposited in melt-out depressions. The depressions had initially functioned as closed depressions and had formed a local base level. They were incorporated into a valley network presumably at the end of the Vistulian glaciation. Blocks of dead ...
© 2017 Elsevier B.V. Closed depressions (CDs) are typical geomorphological features of the loess bel...
Well developed NE-SW trending corridors of outwash in NE Poland are associated with a series of lake...
The depositional conditions of kame terraces in a mountain valley were analysed sedimentologically a...
In the central part of the Rawka lobe of the Warta stage ice sheet of the Middle Polish glaciation (...
Closed depressions (CDs) are common forms occurring in the European loess belt. So far, investigatio...
A sedimentary succession in a gravel pit at Niedźwiedziny was investigated in order to determine it...
The central part of the Woźniki-Wieluń Upland is characterised by mature old glacial landforms assoc...
The article analyses the southern part of the expansion of the Bzura-Ner Spillway (Bzura-Ner Pradoli...
The author attempts at formulating a synthetic description of geological and geomorphological effect...
Closed depressions (CDs) are landforms typical for loess areas. 1761 CDs have been inventoried withi...
The conditions existing in the Uniejów Basin were favourable to formation of outflow after successiv...
Closed depressions in Central Poland are different origin. Two main groups are anthropogenic and na...
Kame terraces in the territory of Lithuania are found in the Late Nemunas glaciation Baltija stage r...
An exceptional concentration of almost identical depressions exist near the small towns of Krotoszy...
The glaciomarginal zone in front of the Opava Mountains (Eastern Sudetes) shows complex relief. This...
© 2017 Elsevier B.V. Closed depressions (CDs) are typical geomorphological features of the loess bel...
Well developed NE-SW trending corridors of outwash in NE Poland are associated with a series of lake...
The depositional conditions of kame terraces in a mountain valley were analysed sedimentologically a...
In the central part of the Rawka lobe of the Warta stage ice sheet of the Middle Polish glaciation (...
Closed depressions (CDs) are common forms occurring in the European loess belt. So far, investigatio...
A sedimentary succession in a gravel pit at Niedźwiedziny was investigated in order to determine it...
The central part of the Woźniki-Wieluń Upland is characterised by mature old glacial landforms assoc...
The article analyses the southern part of the expansion of the Bzura-Ner Spillway (Bzura-Ner Pradoli...
The author attempts at formulating a synthetic description of geological and geomorphological effect...
Closed depressions (CDs) are landforms typical for loess areas. 1761 CDs have been inventoried withi...
The conditions existing in the Uniejów Basin were favourable to formation of outflow after successiv...
Closed depressions in Central Poland are different origin. Two main groups are anthropogenic and na...
Kame terraces in the territory of Lithuania are found in the Late Nemunas glaciation Baltija stage r...
An exceptional concentration of almost identical depressions exist near the small towns of Krotoszy...
The glaciomarginal zone in front of the Opava Mountains (Eastern Sudetes) shows complex relief. This...
© 2017 Elsevier B.V. Closed depressions (CDs) are typical geomorphological features of the loess bel...
Well developed NE-SW trending corridors of outwash in NE Poland are associated with a series of lake...
The depositional conditions of kame terraces in a mountain valley were analysed sedimentologically a...