See how many independent measurements are combined before warnings are issued.
Volcano monitoring does not predict every eruption perfectly. Instead, scientists watch for changes in earthquake activity, ground shape, gas, temperature, and other signals that may show magma moving underground.


Moving magma can crack rock and change volcanic earthquake patterns.
Learn MoreMagma can cause a volcano to swell or shift.
Learn MoreChanges in sulfur dioxide, carbon dioxide, and other gases can provide clues.
Learn MoreThermal cameras and satellites can detect warmer surfaces.
Learn MoreWebcams document ash plumes, lava, snow, weather, and visible changes.
Learn MoreSatellites monitor remote volcanoes across large regions.
Learn MoreVolcano observatories combine instruments with geology and fieldwork.
Learn MoreAgencies use alert systems to communicate changing hazard conditions.
Learn MoreSeismometers detect tiny vibrations people cannot feel.
GPS, tiltmeters, radar satellites, and surveying methods measure movement.
Scientists sample vents, use instruments on the ground, and observe gas from aircraft or satellites.
Heat changes may indicate new lava, hot gas, or changing hydrothermal activity.
Time-lapse imagery can reveal gradual processes.
They can detect ash clouds, heat, deformation, and gas.
Scientists compare present signals with a volcano's known past behavior.
Exact terminology differs by country and aviation authority.