Differentiation of the intensity of accumulation of the Vistulian loesses in Poland and Hungary
DOI:
https://doi.org/10.26485/BP/1986/31/19Słowa kluczowe:
stratygrafia lessów, akumulacja lessu, obszary naddunajskie, południowa Polska,Abstrakt
Indices of the intensity of accumulation of the basie stratigraphical units of the Vistulian loesses have been determined on the basis of dating with the thermoluminescence method. The intensity of accumulation in the upper pleniglacial, preceded by the interpleniglacial amelioration of climate was 10 times stronger than at the early glacial and about 5 times greater than in the !ower pleniglacid. The rhythm of changes of the accumulation intensity was similar in the both areas compared, that is, was conditioned by the factors determining general evolutional rhythm in the glacial cycle. The intensity of loess accumulation in the Danubian areas in central Hungary was much better pronounced than in southern Poland due to the fact that the Danube carried off great quantities of the source materiał for loess formation from other regions of Europe.
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