“…Thus far, most of the experimental work carried out in this emerging discipline has been conducted in glacial environments, work dealing with the movement and orientation of objects on thawing slopes (Harris et al, 2001) or due to solifluction processes, which cause an anisotropic diffusion of materials (Harris et al, 1997;Todisco et al, 2000;Hugenholtz and Lewkowicz, 2002;Lenoble et al, 2008). Geomorphic observations and experiments in glacial contexts have also focused on sorted patterned grounds, regarding the formation of polygons, stripes and stone-banked solifluction lobes (Washburn, 1979;Williams and Smith, 1989;Harris et al, 1993;Todisco et al, 2000;Matsuoka et al, 2003;Kessler and Werner, 2003;Bertran et al, 2010), as well as on documenting these processes in archaeological contexts (Wilson and Clark, 1991;Lenoble et al, 2008;Bertran et al, 2010). The orientation of till fabric has received a substantial amount of attention in structural geological studies.…”