“…In general, seismic networks can i) detect mass wasting activity, ii) locate and track the process in space, and iii) infer kinetic and anatomic details of a process event. The application fields of environmental seismology (Burtin et al ., 2014; Larose et al ., 2015) comprise, for example, time‐resolved investigation of the evolution of slope instabilities (e.g., Mainsant et al ., 2012; Schöpa et al ., 2018), detection and quantification of event activity from the catchment to the global scale (e.g., Dammeier et al ., 2011; Ekström and Stark, 2013; Fuchs et al ., 2018; Lacroix and Helmstetter, 2011), tracking of mass movements in space (e.g., Burtin et al ., 2016; Cook et al ., 2018; Pérez‐Guillén et al ., 2019; Walter et al ., 2020), inversion of seismic signals for event kinetics (e.g., Allstadt, 2013; Ekström and Stark, 2013), and attribution of events to drivers and triggers (e.g., Burtin et al ., 2013; Dietze et al ., 2017; Helmstetter and Garambois, 2010).…”