Litologiczny wskaźnik przemieszczeń materiału skalnego jako element oceny podatności stoków na osuwanie

Abstract

The use of multi-temporal LIDAR data in the study of landslides gives many possibilities. The increasing-over-timeavailabilityofALSdataencouragedresearchondevelopmentoflandslidesusingDifferentialDigital Terrain Models. An important passive factor that determines the development of landslides (especially in the Carpathians) is lithology. The author propose a new lithological displacement index, that dscribes the volume of displaced ground (m3) per area of 1 m2 of a given lithological unit. The example of the test area of Ro¿nowskie Lake has shown that lithological displacement index can assess the landslide susceptibility, which is variable and depends on the amount of rainfall. During periods of heavy rainfall, large volumes of displaced rock masses were recorded in the thick-bedded formations. In dry periods, the trend is reversed.