The measurement and analysis of acoustic emissions is a non-destructive, passive-monitoring technique that is used to determine changes in the physical and chemical conditions of a rock. An acoustic emission (AE) is defined as a transient elastic wave generated by the rapid release of energy within a material (Lockner, 1993;Scruby, 1987). After energy release, AE emanates from the location, or zone, of abrupt and localized mechanical and interfacial energy that triggered the generation of the elastic waves (Scruby, 1987). In geophysics, acoustic emissions methods have been used to monitor crack initiation, coalescence, and propagation (Lockner, 1993), shearing behavior along fractures (Bolton et al., 2020;Rouet-Leduc et al., 2018), and the evolution of drying fronts (Moebius et al., 2012). More recently, acoustic emissions from transportable sources have been used to