“…The vast majority of them come from orbiters; some come from landers and rovers. They contain various geological units and structures from sedimentary, volcanic, tectonic, and impact origin gathered from the United States Geological Survey maps of Mars (Tanaka et al, 2005(Tanaka et al, , 2014, the NASA/International Cartographic Association (ICA) Integrated Database of Planetary Features (Hargitai, 2016; more information on the data and their authors can be found at planetarydatabase.wordpress.com), the NASA Mars Crater Database (Robbins & Hynek, 2012), and individual sources (Bleacher et al, 2007(Bleacher et al, , 2009Carter et al, 2013;Dohm et al, 2000;Ehlmann & Edwards, 2014;Farmer, 1996;Hauber et al, 2013;Hynek et al, 2010;Irwin & Grant, 2009;Malin & Edgett, 2000;Malin et al, 2010;Marzo et al, 2010;Metz et al, 2009;Osterloo et al, 2010;Richardson et al, 2013). Among these sites, the geological units do not necessarily contain any interesting targets, because some correspond to a mixture of undifferentiated rocks at the considered resolution and others stand in dusty areas.…”