Reliktowe osuwisko w Zajączkach Drugich-Łękawicy koło Krzepic (Wyżyna Woźnicko-Wieluńska)

Abstract

This article pre-sents the preliminary results of research on the relict landslide in Middle Jurassic clays. Field mapping, analysis of the Di-gital Elevation Model created from the laser scanning (LiDAR) and orthophotomap was made. It allowed to determine the morphological characteristics of the landslide. We tried to identify the main factors affecting mass movement and to de-termine the probable age of this process. Studied landslide belongs to a larger complex of similar forms. These are forms, pro-bably developed in the Late Pleistocene periglacial conditions, although we can not rule out the Holocene age. Landslide presented in article is due to the size the unique form in the highland-lowland part of the Silesian Voivodeship.