Over the past few days, an earthquake swarm has shaken the supervolcano that lies beneath Yellowstone National Park. Between February 8 and February 18, the region experienced over 200 earthquakes, according to the United States Geological Survey. This might sound super scary, especially if you’ve read that this caldera could cause a volcanic winter when it erupts.

But since we’ve all experienced more than enough existential dread this month, let’s get one thing straight: The Yellowstone Caldera is not about to erupt, and it is not about to blanket the United States in lava and ash because of a seemingly large number of earthquakes.

For one thing, this earthquake swarm — a flurry of small quakes without one large initiating quake — is not a new phenomenon. In 2017, Yellowstone experienced a similar swarm, and experts say this swarm could just be lingering seismic activity from last year. According to the National Parks Service, earthquake swarms in Yellowstone are “common”: the largest happened in 1985 when over 3,000 earthquakes shook the northwest side of the park over the span of three months. It didn’t trigger any volcanic explosions then, and it will not now, say scientists.

Upper terraces of Mammoth Hot Springs, Yellowstone National Park, Wyoming. Hot water is the creative force of the terraces. Even though Mammoth Hot Springs lie north of the caldera ring-fracture system, a fault trending north from Norris Geyser Basin, 21 miles (34 km) away, may connect Mammoth Hot Springs to the hot water of that system. A system of small fissures carries water upward to create approximately 50 hot springs in the Mammoth Hot Springs area. Another necessary ingredient for terrace growth is the mineral calcium carbonate. Thick layers of sedimentary limestone, deposited millions of years ago by vast seas, lie beneath the Mammoth area. As ground water seeps slowly downward and laterally, it comes in contact with hot gases charged with carbon dioxide rising from the magma chamber. Some carbon dioxide is readily dissolved in the hot water to form a weak carbonic acid solution. This hot, acidic solution dissolves great quantities of limestone as it works up through the rock layers to the surface hot springs. Once exposed to the open air, some of the carbon dioxide escapes from solution. As this happens, limestone can no longer remain in solution. A solid mineral reforms and is deposited as the travertine that forms the terraces. Photo credit: Brocken Inaglory via Wikimedia Commons commons.wikimedia.org/wiki/File:Upper_Terraces_of_Mammoth...
Hot springs in Yellowstone lie north of the caldera system.

The last time this supervolcano erupted was over 70,000 years ago. In the time that modern scientists have been studying it, they’ve concluded that Yellowstone, even though it sits on top of a giant well of subterranean lava and experiences 1,000 to 3,000 earthquakes a year, has extremely low odds of erupting.

If there is going to be an eruption, geologists will be able to tell well in advance. USGS scientists say the current flurry of quakes is not a warning of an impending eruption.

Since the park experiences earthquakes so frequently, the fact that this swarm has yielded so many small quakes should not be worrisome. Add to that the fact that they really are tiny quakes, and our fears should be put to rest. The largest earthquake in this swarm has only registered a magnitude of 2.9, making it a very weak earthquake. To put it simply, you might not feel a 2.9 earthquake if you’re standing where it happened. Additionally, the quakes have been dozens of miles below the Earth’s surface.

So, for anyone who’s worried that the Yellowstone supervolcano will end life as we know it, there’s no need to worry. But if you were hoping it would put a quick end to our misery, take comfort in the fact that there’s probably another existential threat right around the corner.