Mount St. Helens' high frequency of eruptions during the recent geologic past and its two eruptive episodes of the past three decades indicate a high probability of renewed eruptive activity.
Mount St. Helens has produced four large explosive eruptions during the past five centuries that affected the Pacific Northwest region and sent large amounts of volcanic ash downwind. Owing to these factors, USGS maintains a robust monitoring program at the volcano to detect signs of renewed unrest and works with Federal, State, and local agencies to develop crisis plans and risk-mitigation strategies. Businesses and citizens should be aware of potential future hazards and consult with local emergency-management agencies for advice on how to prepare for volcano and other types of natural hazards.
Among the possibilities for renewed activity at Mount St. Helens are resumption of lava-dome growth, eruption of basaltic or andesitic tephra and lava flows, explosive eruptions of dacitic tephra and pyroclastic flows, and large lahars that sweep down valleys heading on the volcano.
Hazards from Post-Eruption Excess Sediment at Mount St. Helens
Ash Cloud Simulations - What if Mount St. Helens Produced an Explosive Eruption Today?
Mount St. Helens' high frequency of eruptions during the recent geologic past and its two eruptive episodes of the past three decades indicate a high probability of renewed eruptive activity.
Mount St. Helens has produced four large explosive eruptions during the past five centuries that affected the Pacific Northwest region and sent large amounts of volcanic ash downwind. Owing to these factors, USGS maintains a robust monitoring program at the volcano to detect signs of renewed unrest and works with Federal, State, and local agencies to develop crisis plans and risk-mitigation strategies. Businesses and citizens should be aware of potential future hazards and consult with local emergency-management agencies for advice on how to prepare for volcano and other types of natural hazards.
Among the possibilities for renewed activity at Mount St. Helens are resumption of lava-dome growth, eruption of basaltic or andesitic tephra and lava flows, explosive eruptions of dacitic tephra and pyroclastic flows, and large lahars that sweep down valleys heading on the volcano.