Major VEI 6+ eruptions occur roughly once every 50–100 years on average, with the most recent example being Pinatubo in 1991. As of mid-August 2026, global monitoring from the Smithsonian Global Volcanism Program and USGS shows approximately 40 ongoing eruptions, all at low to moderate levels with no reported unrest or precursory signals capable of rapid escalation to VEI 6 thresholds (roughly 10 km³ ejecta). Historical records and eruption frequency data indicate such events require extended magma chamber pressurization rarely completed within a single calendar year. Trader consensus at 95%+ for “No” aligns with this absence of observable triggers and the short remaining timeframe. Unexpected developments, such as rapid intensification at a high-risk system like Taal or an Indonesian arc volcano, remain possible but statistically remote given current seismic, deformation, and gas data.