1996
DOI: 10.1127/zfg/40/1996/271
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“…1). During the last glaciation, under periglacial climate conditions, intensive aeolian processes took place in this zone and inland dunes and aeolian cover sands were formed (LANDSBERG, 1956;MAARLEVELD, 1960;KOSTER, 1982KOSTER, , 1988RUEGG, 1983;SCHWAN, 1987SCHWAN, , 1988BÖSE, 1991;KOLSTRUP, 1991;VANDERBERGHE, 1991;LIEDTKE, 1993;MYCIELSKA-DOWGIAŁŁO, 1993;KASSE, 1999KASSE, , 2002KASSE ET AL., 2007; VANDERBERGHE ET AL., 2013; KALIŃSKA-NARTIŠA . The aeolian landscape of this part of Europe has a Late Glacial origin and, to a lesser extent, Holocene origin.…”
Section: Introductionmentioning
confidence: 99%
“…1). During the last glaciation, under periglacial climate conditions, intensive aeolian processes took place in this zone and inland dunes and aeolian cover sands were formed (LANDSBERG, 1956;MAARLEVELD, 1960;KOSTER, 1982KOSTER, , 1988RUEGG, 1983;SCHWAN, 1987SCHWAN, , 1988BÖSE, 1991;KOLSTRUP, 1991;VANDERBERGHE, 1991;LIEDTKE, 1993;MYCIELSKA-DOWGIAŁŁO, 1993;KASSE, 1999KASSE, , 2002KASSE ET AL., 2007; VANDERBERGHE ET AL., 2013; KALIŃSKA-NARTIŠA . The aeolian landscape of this part of Europe has a Late Glacial origin and, to a lesser extent, Holocene origin.…”
Section: Introductionmentioning
confidence: 99%