Continuous seismograms are time series of the ground motion recorded at a single location and provide a vast amount of information about processes occurring at the Earth's surface and interior. The recorded ground motion at a given location results from the convolution of the medium's impulse response-expressed as the Green's function-and the seismic waves emitted by various sources, often simultaneously. Thus, continuous seismograms are goldmines to study the medium's properties or sources in time. However, unmixing source or medium changes is often not easy, especially if source and medium changes coincide. For instance, seismic recordings in the vicinity of volcanoes, where many different source and medium effects occur, are challenging and complex datasets to analyze.To better explore continuous seismic data, seismologists developed many data processing tools to extract valuable information for the task at hand. For example, the short-term-average to long-term-average energy ratio (STA/ LTA) scans the continuous recordings for impulsive signals (Allen, 1978). On the other hand, passive image interferometry can interrogate the medium regularly by exploiting the ambient seismic signals of a data set (Sens-Schönfelder & Wegler, 2006). Undoubtedly, these tools delivered many new insights into the processes happening at and inside the Earth. However, it is important to note that the design of the tools and the related preprocessing favors certain processes in the seismic data. This can be a problem if the source or medium processes encoded in the seismic data are poorly understood. For example, non-volcanic tremors were detected about 20 years ago (Obara, 2002), and still today, the physical mechanism and signal properties of such events are not well apprehended. Therefore, it remains unclear if these signals do not exist in specific environments or if the detection tools are not adapted to the task (Bocchini et al., 2021;Pfohl et al., 2015).Artificial intelligence (AI) can help overcome those blind spots and discover new signals or hidden patterns within the data. Recently, clustering gained attention as a method to identify families of signals in the continuous seismograms (