“…The second method uses the fundamental geological properties of the artefact to predict a potential origin in the absence of comparative material (Freestone et al, n.d.). The former method relies on the existing chemical and isotopic data collected from various Roman glass assemblages, such as the composition of glass collected from the Roman furnaces in Egypt (Nenna et al, 2000); the small scale production from York, England (Bingham and Jackson, 2008;Jackson et al, 2003b); or the detailed evidence from the 4 th century glass possibly made at Hambach, Germany (Wedepohl and Baumann, 2000;Wedepohl et al, 2011a); as well as the detailed studies undertaken on 4 th -5 th century HIMT glass and 4 th -8 th century Levantine glass (Freestone, 2001;Freestone et al, 2002b). The second method utilises isotopic studies, particularly of Sr and Nd, to infer the likely locations of glassmaking sands and therefore the location of the primary furnaces in which the raw glass was made (Freestone et al, n.d.).…”