“…As such, there is an interdependence between the direction of the rockfall trajectory in the x,y domain, the kinematics of the falling rock, its rebound positions and heights and if included, impacts on trees. Examples of such models are EBOUL-LMR (Descoeudres and Zimmermann, 1987), STONE (Guzzetti et al, 2002), Rotomap (Scioldo, 2006), DDA (Yang et al, 2004), STAR3-D (Dimnet, 2002), HY-STONE and Rockyfor3-D , RAMMS:Rockfall (Christen et al, 2007); Rockfall-Analyst (Lan et al, 2007), PICUS-ROCKnROLL (Rammer et al, 2007;Woltjer et al, 2008) or as shown in Masuya et al (1999). The major advantage of 3-D models is that diverging and converging effects of the topography, as well as exceptional or surprising trajectories, i.e., those that are less expected at first sight in the field, are clearly reflected in the resulting maps.…”