摘要：Since 2014 Jan Kochanowski University in Kielce participate in the research in Paphos region in SW Cyprus. The
aim of geomorphologic study was the age and sediments of terraces and floodplains in Ezousas river valley. Results
of TL dating indicate distinct differentiation in fluvial activity in the Late Pleistocene and Holocene. Two main
alluviation phases were distinguish: 75-48 ka and 25-13 ka. Relief and the varied tectonic movements had a great
impact on the valley formation and alluvial features.
