“…Our knowledge of specific source areas is still quite variable. Recent geological and geophysical surveys of Göllüdag (Binder et al, 2011), Nemrut Dağ (Robin et al, 2015;Robin et al, 2016), north-east Anatolia (Chataigner andGratuze 2014a, 2014b; see http://geobs.univ-rouen.fr/; Akköprü et al, 2017), Meydan Dağ and elsewhere by the McMaster Obsidian Procurement Expedition (see https://maxlab.mcmaster.ca/research-projects/mcmaster-obsidian-procurement-expedition-mope), as well as Biagi and Gratuze's survey of Paravani /Chikiani in Georgia (Biagi and Gratuze, 2016), demonstrate that the physical availability of obsidian as well as its elemental composition is often considerably more complicated than initially appreciated (cf., Shackley, 2008;Poupeau et al, 2005;Binder et al, 2011;Robin et al, 2016). In many cases, it is clear that the locations from which people obtained obsidian in the past were the geological outcrops themselves, as the quarry workshops at the Göllüdağ source indicate (Binder et al, 2011), but in other cases obsidian was probably mainly obtained from secondary sources such as river beds.…”