Most of the seismicity worldwide stems from the brittle failure of rock due to tectonic forces. However, other types of seismicity are also common in environments such as glaciers, geothermal systems, and active volcanoes. While brittle failure earthquakes occur in these areas, pressure changes in fluid-filled cavities can produce other types of signals. At volcanoes, LP events, as a low-frequency signal with the resonant property, have been interpreted to be the far-field seismic response of oscillations of fluid-filled cavities during fluid transport, and therefore, it serves as an important eruption precursor (