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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