Earthquakes frequently occur before volcanic eruptions, acting as one of the most important early warning signs of rising magma and pressure inside a volcano. These seismic events can cluster around active volcanic zones and help scientists monitor changes in a volcano’s internal state.
The time gap between increased seismic activity and an actual eruption can vary greatly, from just a few hours to many months. Because of this range, seismologists track not only the number of quakes but also their depth, magnitude, and location relative to the volcano.
In some documented cases, a sharp increase in shallow earthquakes has been detected only hours before an eruption, indicating rapid magma ascent. In other situations, a long-lasting swarm of low- to moderate-magnitude quakes has persisted for weeks or months before any eruptive activity took place.
This variability means that a single earthquake near a volcano does not automatically imply an imminent eruption; instead, specialists look for patterns over time. Continuous monitoring networks around active volcanoes combine seismic data with gas emissions, ground deformation, and thermal information to improve eruption forecasts.
Most seismic activity associated with volcanoes is directly or indirectly linked to the movement of magma and volcanic fluids within the crust. As magma intrudes into surrounding rock, it can fracture the rock and generate swarms of small to moderate earthquakes.
These volcano-related earthquakes often occur at relatively shallow depths compared with many tectonic earthquakes, reflecting processes in the upper crust. Their characteristics, such as harmonic tremor or long-period events, can differ from typical tectonic quakes and provide additional clues about subsurface magmatic processes.
Earthquakes often precede volcano eruptions, sometimes only by hours and other times by several months. While most seismic activity related to volcanoes is linked to magma movement, its timing and intensity can vary widely.
Earthquakes near active volcanoes serve as key precursors to eruptions, but highly variable timing from hours to months demands continuous, pattern-based monitoring rather than reliance on single events.