The strong market consensus favoring no VEI ≥6 eruption in 2026 stems primarily from the events' extreme rarity, with global recurrence intervals estimated at decades to centuries for VEI 6 and roughly 500–1,000 years for VEI 7, based on geological records and sulfate deposition data. As of mid-August 2026, Smithsonian and USGS monitoring reports document dozens of ongoing but modest eruptions worldwide—such as at Kīlauea, Etna, and various Indonesian and Philippine sites—without the sustained deep seismicity, rapid deformation, or precursory signals that typically precede colossal events. Remaining months offer limited time for escalation at monitored systems. A sudden shift could occur only if a high-magnitude unrest episode develops rapidly at a large caldera, though historical patterns indicate such rapid transitions to VEI ≥6 remain exceptionally uncommon.