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  • This study is an attempt to establish the relationship between morphoscopic surface features of quartz-grains and the dynamic processes of debris flows. More specifically, it is aimed at distinguishing between quartz-grain surface characteristics
  • for a paleo-liquefaction event is discussed. Sedimentologic and morphoscopic analyses both provided the necessary elements and parameters to link the ca. 4 m deep sandy layers to the 2009 sand blows on the ground surface as well as to the paleo-liquefaction