As already explained in chapter 2, this book, without claiming completeness, deals primarily with landslides in stratified soils. With only a few exceptions, these are soils from the younger Tertiary; they are frequently marine sediments originating from the Sarmate (uppermost Miocene) and the Pont-Pannon (lowest Pliocene).
KeywordsShear Strength Earth Pressure Slip Surface Residual Strength Sand Layer
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