“…Raman spectroscopy is a non‐destructive analytical tool used to obtain chemical and structural information on melts, glasses, and mineral crystals within the Earth and planetary sciences (e.g., Angel et al., 2012; Cicconi et al., 2022; McMillan & Wolf, 1995; Mysen, 1983; Nasdala et al., 2004; Neuville et al., 2014; Rossano & Mysen, 2012; Seifert et al., 1982); including natural glasses such as volcanic glass (Di Genova et al., 2015; Dingwell, 2003; Giordano, González‐García, et al., 2020; Giordano, Russell, et al., 2020), fulgurites (Alte da Veiga et al., 2021; Carter, Hargreaves, et al., 2010, Carter, Pasek, et al, 2010; Cicconi et al., 2022), and impactites (Gucsik et al., 2004; Ostroumov et al., 2002; White & Minser, 1984). Raman spectroscopy has also been used in more recent studies to estimate the iron oxidation state (Di Genova et al., 2016; Di Muro et al., 2009; Le Losq et al., 2019; Magnien et al., 2006; Roskosz et al., 2008), water abundance (Behrens et al., 2006; Le Losq et al., 2012; Mercier et al., 2009, 2010; Schiavi et al., 2018; Thomas et al., 2008), and carbon dioxide content (Morizet et al., 2009, 2013) within synthetic and natural glasses.…”