Zapis peryglacjału w środkowo-wschodniej Irlandii
DOI:
https://doi.org/10.26485/BP/1981/28/6Słowa kluczowe:
pseudomorfozy po klinach lodowych, krioturbacje kongeliflukcja, tory, epizody peryglacjalneAbstrakt
W środkowo-wschodniej Irlandii można rozpoznać różnorodne zjawiska peryglacjalne związane z dwoma, a być może trzema, epizodami chłodnego klimatu. Jedynie ostatnie z tych wydarzeń można datować z pewną dokładnością, ze względu na niepewność co do długości okresu reprezentowanego przez osady lodowcowe, które stanowią ramy chronologiczne względne.
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