Seismic monitoring plays a fundamental part in mitigating hazards at volcanoes. During periods of unrest, thousands of earthquakes can occur each day, producing a diverse range of seismic signals that reflect a multitude of interlinked volcanic processes (e.g., migrating fluids, fault movement, explosions, rockfalls). These earthquakes are generally recorded by broadband seismometers, which are highly sensitive to ground motion across a wide range of frequencies and record signals at high sample rates (typically 100 times or more per second). This level of detail, however, comes at the cost of generating vast amounts of data. Many seismic networks utilize tens or even hundreds of seismometers at a given time (e.g., Hansen & Schmandt, 2015), making real-time manual inspection of these time series practically infeasible. Previous