
In his movie 2012, Roland Emmerich’s 2009 love letter to the Mayan apocalypse, our heroes barely manage to escape Yellowstone National Park before it explodes beneath them. This not-so-subtle sci-fi sequence is actually based on something real: the Yellowstone supervolcano. What distinguishes this kind of volcano from regular volcanoes, and what will happen if—or when—it erupts?
Regular vs. Super Volcano
Mount St. Helens, a stratovolcano, erupted in 1980. | Historical/GettyImagesThere are four main types of volcanoes: Cinder cones, composite or stratovolcanoes, shield volcanoes, and lava domes, which all rise above the earth. But supervolcanoes like the one under Yellowstone are calderas: vast sunken areas formed when the volcano expels all of its magma, and the land comes back to rest in the empty chamber. These calderas can be as big as 60 miles across (the current Yellowstone caldera, which sits on several older calderas, measures about 30 miles by 45 miles).
When Mount St. Helens, a stratovolcano located in Washington, erupted in 1980, the event rated a 5 on the Volcanic Explosivity Index (VEI) and expelled one cubic kilometer of ash. But supervolcanoes register 8 on the VEI and typically expel 10,000 times that volume of magma and ash. The most recent Yellowstone eruption, which occurred 630,000 years ago, released 240 cubic miles of volcanic debris.
The Yellowstone supervolcano is just one of several scattered around the globe. An incomplete list includes Taupo in New Zealand, which last erupted in the 3rd century CE. Before that was a supereruption of Toba in Sumatra, Indonesia, which occurred 74,000 years ago. There’s a supervolcano near Pompeii, and one in Chile, too. There may be more we haven’t yet discovered.
What Happens If A Supervolcano Erupts?
Yellowstone's geothermal pools indicate there's a sleeping supervolcano underground. | George Rose/GettyImagesBeneath Yellowstone's surface—sometimes as shallow as 5 or 6 miles—is a reservoir of solid rock and magma. Below that lies a 45-mile-wide plume of molten rock originating from at least 410 miles beneath the Earth's surface. This plume powers Yellowstone's remarkable geysers and geothermal pools. Bob Smith, who first described Yellowstone as 'a living, breathing caldera' in 1979, states in his book 'Windows into the Earth' that if the caldera were to erupt, 'devastation would be complete and incomprehensible.'
Initially, there would be swarms of earthquakes, followed by a massive explosion that would obliterate Yellowstone. Clouds of ash and gas would incinerate everything in their path. Ash would blanket most of North America, destroying food sources. Some speculate that a supereruption from the Yellowstone caldera would instantly kill 87,000 people. Others suggest that such an eruption would lower the Earth's temperature by at least 21 degrees and might even block out the sun.
A study determined that if or when Yellowstone next erupts, it will probably be centered in one of three parallel fault zones running north-northwest across the national park.
Nonetheless, there's likely no cause for concern. Statistically, supereruptions occur at a rate of approximately 1.4 per million years. According to the U.S. Geological Survey, the probability of Yellowstone erupting in any given year is minimal: about one in 730,000, or 0.00014%.
