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Table 1

Sedimentological parameters of the Holocene deposits in the Morsott area. The sedimentological parameters determined to the fine fraction, less than 2 mm, show variable mode, average, index asymmetry, and flattening values indicating a medium to high energy carrier current regime at the base of the series (unit K and L) and from medium to low during the Holocene.

Designations Breccias and pebbles set Silty sands set Sandy clayey silts set Sandy silts set  
Units D, L K, E C, F, H, J A, B, G, I  
Mode in μm 500 350 380 400 Characteristics
Mean in μm 380 200 115 250 What reveals that the current transport has an average with weak energy
Sorting So −0.1 −0.9 −0.5 −0.35 Grains very well classified
Skewnes Sk −0.3 −0.42 −0.50 −0.45 The classification is better beside the fine particles
Kurtosis Ku 0.3 0.1 0.1 0.2 The curves are very platykurtic with heterogeneous composition
Classification according to Folk (1954) Silty facies Silty facies Silty facies Silty facies  

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