“…(2020) found that the fragment size distribution defined two power‐law trends (two slopes, or D ‐values, in a log‐log plot) that intersect at a value of = ∼10 μm (Figure 4). Such “bifractal” distributions are observed in a wide range of different processes from drilling, brecciation, crushing, and milling of rock (Barnett, 2004; Carpinteri & Pugno, 2002; Farris & Paterson, 2007; Roy et al., 2012; Taşdemir, 2009) to rapid shock fragmentation of brick, glass, quartz, rock and ceramic (Barnett, 2004; Capaccioni et al., 1986; Davydova et al., 2014; Fujiwara et al., 1977; Hossain & Kruhl, 2015; Keulen et al., 2007; Roy et al., 2012; Suteanu et al., 2000). Bifractal distributions are sometimes interpreted as identifying a grinding limit (e.g., Keulen et al., 2007), but 10 μm is far too large for the grinding limit of garnet (∼0.26 μm for almandine‐pyrope; B. R. Song, Johnson, Song, et al., 2020).…”