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They don't care about the motion of tectonic plates, so they can break the crust to create volcanoes in the middle of nowhere that stubbornly stay active as the crust shifts around them.
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Scientists love to put big booms on a scale and came up with a logarithmic scale that measures the volume ejected during an eruption.
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Simply put, it starts really small and gets very big very quickly.
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A VEI 2 eruption would fill 400 full Olympic swimming pools with lava.
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We have around 10 of these per year.
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At VEI 3, we already see devastating effects like the eruption of the Semeru volcano in 2021 that destroyed thousands of homes in Indonesia.
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At VEI 5, we see catastrophic amounts of materials, cubic kilometers of debris, equivalent to an entire lake of molten rock blasted into the air.
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At a VEI of 6, an eruption can change the world.
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In 1883, the Indonesian island volcano Krakatoa erupted nearly continuously over the course of five months.
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One of those eruptions blew it apart, producing the loudest sound recorded in history.
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30-meter high tsunamis swept away nearby populations and so much gas and ash were released, the global temperatures cooled by nearly 0.5 degrees Celsius.
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Red, dusty sunsets followed for many years.
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At VEI 7, we get supercolossal eruptions, millennium-defining events that human civilization has only encountered a handful of times.
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Mount Tambora was a 4,300-meter high mountain until it exploded in 1815 and released 400 times more energy than the Tsar Bomba.
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140 billion tons of ash and dust were shot halfway to space before smothering the world's skies, turning them a sickly yellow.
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There was no summer the following year, crops died, and over 100,000 people perished.
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This is the dreadful potential of volcanic eruptions, with famines across the other side of the world and even centuries-long cold periods being attributed to them.
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Okay, but what's a supervolcano?
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The term supervolcano is a media invention and not a scientific term.
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The main issue with them is that not every eruption from a supervolcano is a supereruption.
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What makes supervolcanoes special is that they've been waiting to erupt for hundreds of thousands of years.
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Pressure builds up in colossal magma reservoirs several kilometers deep until it becomes strong enough to lift the rock above it by several meters.
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Rocks crack under the pressure until they finally give way and billions of tons of gas and ash blast out at supersonic speed.
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And yet, that is only a small portion of the magma reservoir.
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Supereruptions are like a boiling pot of water popping its lid off and spitting a bit off the top.
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Afterwards, the ground collapses into the void left behind, forming a hole called a caldera.
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Under this caldera, pressure starts building again until the volcano gathers enough energy for another supereruption.
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But this could take hundreds of thousands of years.
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It's estimated that one of the few volcanoes capable of supereruptions on Earth could cause a catastrophic eruption every 17,000 years on average.
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That would make them far more frequent than comparable asteroid impacts.
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The most recent supereruption is the Oranui eruption 26,500 years ago in New Zealand.
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With the force of dozens of billions of tons of TNT, a Mount Everest-sized pile of explosives, a huge portion of the landscape was scooped out and thrown into the atmosphere.
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It left behind a caldera spanning 20 kilometers, and it caused the entire southern hemisphere to undergo a period of abrupt cooling.
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Though among supereruptions, it's a mere firework.
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The Lake Toba eruption of 74,000 years ago was a much more significant turning point in history.
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It released a gargantuan 5,300 cubic kilometers of material, enough to blanket parts of South Asia in 15 centimeters of ash and trigger a rapid 4 degrees Celsius drop in global temperatures.
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It's possible that the volcanic winter lasted 10 years, followed by worldwide droughts for centuries.
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Earth's climate might have not recovered for a thousand years.
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The largest volcanic events we know of were not really huge explosions, but floods of millions of cubic kilometers of lava.
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The grand finale were the Siberian Traps around 250 million years ago, a continuous release of lava for 2 million years.
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They raised the ocean temperatures to over 40 degrees Celsius, which caused the Permian-Triassic extinction, killing over 90% of all species.
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Earth's surface needed 9 million years to recover.
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These sorts of eruptions don't change the climate.
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They are the climate.
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But thankfully, we haven't seen anything even remotely close to that scale in many millions of years.
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So, should you be scared of supervolcanoes?
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They've been used to frighten many people and are overhyped as an unavoidable apocalypse.
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The most famous one, Yellowstone, will erupt again, but they will be relatively small eruptions.
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The chance of a VEI8 eruption in the next few hundred years is less than 2%, and more importantly, it wouldn't come as a sudden surprise.
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However, less powerful but more frequent eruptions can also do serious damage to our civilizations and are in many ways a much greater concern.
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So, we must watch for slow changes in magma reservoirs, like ground swelling and temperature increases,
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And there's time to develop solutions that can remove sulfur and ash from the stratosphere to eliminate the root cause of the climate disruption we've seen from previous eruptions.
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Who knows?
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Maybe we'll even be able to turn this force of destruction into an agent for good by exploiting the geothermal energy held in their giant magma reservoirs.
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We've done this work for so many other disasters, and we are already doing things we could only have dreamed about decades ago,
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With determination, humanity really can solve anything.
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So, while deep below us an angry hell is churning and waiting for its moment, you can sleep well tonight.
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Learning how we can get ahead of catastrophes like climate change and supervolcanoes is interesting but can also be challenging.
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Maybe you still feel like you don't really understand how most of the science behind it works.
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And, on your own, it seems too hard to dig deeper.
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To solve this, we've collaborated with our friends from Brilliant to create a series of lessons to build your understanding of fundamental science.
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Brilliant is an interactive learning tool that makes science accessible with a hands-on approach.
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Think of each lesson as a one-on-one deep dive version of a Kurzgesagt video.
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In our latest lessons, you'll discover the mechanisms that drive climate change and use them to understand the impact of supervolcanoes on our global climate.
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Beyond new Kurzgesagt lessons regularly released, Brilliant has thousands of lessons for members to explore.
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With new releases each month, you'll always find something fascinating to learn.
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To get hands-on with Kurzgesagt lessons now, go to brilliant.org/nutshell and sign up for free.
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And with a free trial of Brilliant Premium, you can explore everything Brilliant has to offer.
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There's even an extra perk for Kurzgesagt viewers.
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The first 200 people to use the link get 20% off their annual membership, which unlocks all of Brilliant's courses in maths, science, and computer science.
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We love going down a rabbit hole with our research.
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Brilliant will take you by the hand to come along on the ride.
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Today, we are answering an age-old, very scientific and important question.
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It's more interesting and weird than you probably think.
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Let's start with the basics.
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Why isn't the Moon on its way to crash into us already?
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We know that Earth's gravity pulls everything towards it, including the Moon, but somehow it stays up, as if suspended by some opposite force.
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But there is no other force countering gravity.
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Instead, the trick to staying up is a sideways motion that we call an orbit.
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You see orbits every day.
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When you throw a ball, it makes a tiny little orbit.
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The only difference between the ball's orbit and the Moon's is that the ball eventually hits the ground.
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Basically, the reason is speed.
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If you could throw your ball fast enough, it would bend around the world and come back to you.
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If there were no air slowing it down, it could orbit forever.
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And this is what the Moon does, falling sideways around Earth very fast with no air slowing it down, orbiting Earth every 27 days at 3,600 km an hour.
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So, how do we crash it into Earth?
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In a nutshell, to change an object's orbit, you need to change its speed, which changes where gravity takes it.
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But even small changes require enormous forces, which is why all the large objects in the Solar System are so stable nowadays.
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According to science, the Moon is big and very massive.
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Even igniting billions of rocket engines all over its surface would barely move the Moon.
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It looks like nothing short of magic will make the Moon fall, so we'll use a magic spell that slows down the Moon so much that it changes its orbit and spirals towards Earth.
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To get the most from the experience, the Moon will take exactly one year before it hits Earth.
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For the first few days, nothing really changes.
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The Moon gets a tiny bit brighter, and scientists get confused, but the rest of us don't notice anything different.
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The only noticeable real effect of the Moon on the Earth are the tides.
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Tides exist because while Earth pulls on the Moon, the Moon's gravity pulls back on the Earth.
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Since the strength of gravity gets weaker with distance, different parts of the Earth feel a slightly different pull,
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As Earth rotates every day underneath the Moon, the Moon's influence fluctuates, causing the water level of the oceans to rise and fall by about half a meter twice a day.
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But with the Moon drawing ever closer, high tide gets higher every day.
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