The Yellowstone Caldera—a supervolcano—last had a major eruption 640,000 years ago (Lava Creek Tuff). Current science: no imminent eruption.
Annual probability: <1 in 700,000 (USGS). Monitoring: Seismicity (1,500–2,500 quakes/year, mostly tiny), ground deformation (GPS, InSAR), gas emissions, hydrothermal activity. No anomalous signals indicating magma ascent.
Most likely: Hydrothermal explosion (crater-forming, local) or lava flow (rhyolite/basalt, slow, contained). Least likely but catastrophic: Supereruption (>1,000 km³ ejecta)—global climate impact (volcanic winter), continental ashfall, agricultural collapse. Recurrence interval: ~600,000–800,000 years—we're within range but not overdue.
Volcanoes don't run on schedules. Magma accumulation is episodic. Current magma reservoir is 5–15% melt—too crystalline to erupt en masse. Recharge needed—could take millennia.
Hydrothermal explosions, earthquakes, toxic gas—localized but real. Tourist safety (boardwalks, closures) is the operational focus.
Yellowstone will erupt again—geology guarantees it. But not in our lifetimes, almost certainly. The wonder is that we can monitor a sleeping giant this closely.