Landslides are mass displacements of soil or rock, which move more or less continuous downwards from a scarp along a thin shear zone. In literature two landslide types are distinguished (after Highland & Bobrowsky, 2008).

  • translational landslide
  • rotational landslide

Translational landslides (Fig. 1, left) move downslope in a planar manar, usually along a structural pre-existing, planar shear zone. In contrast, rotational landslides (Fig. 1, right) perform a rotation movement along a concavly curced sliding surface. In this case the regolith is normally more homogenous. Translational slides are among the most common types of landslides worldwide, including Lower Austria. As a general rule, translational slides are more shallow then rotational slides and range from a small scale (size of a single-family house) to larger landslides with several kilometres in length. The process velocity is highly variable and can range between centimetres (and less) over a month to multiple meters per day and even faster. With increasing velocity, the landslide can degrade and change into a flow process e. g. debris or earth flows (Highland & Bobrowsky, 2008).

Within the NoeSLIDE project sliding processes are investigated in Waidhofen a.d. Ybbs (Hofermühle, Eckerwirt), in Gresten (Salcher landslide) and in Brandstatt.




Figure 1: Schematic of a translational landslide (left) and a rotational landslide (right) (Source: Highland & Bobrowsky, 2008).



  • Highland, L. & Bobrowsky, P.T., 2008. The landslide handbook: a guide to understanding landslides, US Geological Survey Reston, VA, USA.