“…Thus, fluvial courses, ephemeral streams, alluvial fans, and erosion/accumulation aeolian processes reach their greatest development (Harvey, 1989;Watson, 1989;Cooke et al, 1993). There is a noticeable interaction between the fluvial systems and the activity of aeolian processes, as described in arid areas of different continents (Bullard and McTainsh, 2003;Forman et al, 2006;Madale et al, 2008;Roskin et al, 2014Roskin et al, , 2017Al-Masrahy and Mountney, 2015;Liu and Coulthard, 2015;Vardi et al, 2018;among others).…”