Abstract
The wide distribution of the Pliocene clays over the territory of Bulgaria and the landslides which appear in them draw the attention of a great number of specialists. Three types of clays may be distinguished: sandy and silty clays, heavy clays with silty seams, and fat clays overlying coal layers. They are water-saturated and show a plastic consistence. With increasing depth, the density decreases and the moisture increases.
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