
The Doorway to the Underworld is Growing and We Can't Stop It
What this covers
Visit https://brilliant.org/scishow/ to get started learning STEM for free. The first 200 people will get 20% off their annual premium subscription and a 30-day free trial.
Batagay (aka Batagaika) Crater goes by many names. Scientists call it a retrogressive thaw megaslump; the internet may know it best as the Doorway to the Underworld. And since it opened up in the Siberian permafrost over half a century ago, it's been getting bigger.
Hosted by: Hank Green (he/him) ---------- Support us for $8/month on Patreon and keep SciShow going! https://www.patreon.com/scishow Or support us directly: https://complexly.com/support Join our SciShow email list to get the latest news and highlights: https://mailchi.mp/scishow/email ---------- Huge thanks go to the following Patreon supporters for helping us keep SciShow free for everyone forever: Odditeas , Garrett Galloway, Friso, DrakoEsper , Kenny Wilson, Lyndsay Brown, Jeremy Mattern, Jaap Westera, Rizwan Kassim, Harrison Mills, Jeffrey Mckishen, Matt Curls, Eric Jensen, Chris Mackey, Adam Brainard, Ash, You too can be a nice person, Piya Shedden, charles george, Alex Hackman, Kevin Knupp, Chris Peters, Kevin Bealer, Jason A Saslow ---------- Looking for SciShow elsewhere on the internet? SciShow Tangents Podcast: https://scishow-tangents.simplecast.com/ TikTok: https://www.tiktok.com/@scishow Twitter: http://www.twitter.com/scishow Instagram: http://instagram.com/thescishow Facebook: http://www.facebook.com/scishow
#SciShow #science #education #learning #complexly ---------- Sources: https://docs.google.com/document/d/1lFwooq8DOsNuPYwouyhQzEONRwGQyft42-qvATOUGMs/pub
Source description (no synthesized summary yet).
The Batagay Crater in Siberia, formed by Soviet deforestation and accelerated by climate-driven permafrost thaw, demonstrates a self-reinforcing feedback loop of environmental degradation while paradoxically serving as an invaluable geological archive revealing 650,000 years of regional climate and fauna history.
- Human activity (forest clearing) initiated permafrost thaw that created a positive feedback loop of melting, exposure, and warming
- The crater's expanding walls expose stratified geological history including preserved megafauna remains, making it a scientific resource despite environmental damage
- The crater will self-limit within decades as it approaches bedrock, but ongoing carbon release and river contamination pose immediate problems
This asset isn't compiled yet
You're seeing its claims, ranked. Compile it to build the argument threads, weight them, and check each claim against your library — the full view.
The Batagay Crater is self-excavating, and each year it reveals new, well-defined cross-sections of its geological history, with geologists able to sample ice structure, sediment composition, and biomass remains from each layer to compile a climate and fauna history stretching back 650,000 years.
“But all that melting permafrost is actually a good thing in one particular way. Basically, the Batagay Crater is self-excavating, and each year it reveals new, well-defined cross-sections of its geological history. At the head of the proverbial stingray, there's a sheer cliff that's 55 meters tall, perfectly exposing the permafrost's layers. Geologists can sample the ice structure, sediment composition, and biomass remains from each layer of the permafrost cake, and compile a history of the region that stretches back 650,000 years.”
The Batagay Crater appeared in the 1960s after Soviets cleared nearby forests to search for minerals, and without tree roots the landscape became more susceptible to erosion, and without tree cover it was easier for the Sun to warm the ground, kicking off a vicious cycle of permafrost melting.
“Like if you could time travel back to the 1960s, you'd find yourself standing in a seemingly harmless ravine. But the Soviets had recently cleared a nearby forest to search for good places to mine a bunch of different minerals. Without tree roots, the landscape became more susceptible to erosion. And without tree cover, it was a lot easier for the Sun to warm the ground. In other words, the sudden lack of trees kicked off a vicious cycle of permafrost melting.”
When higher surface temperatures cause snow covering the upper permafrost layers to melt, the darker newly-exposed layers absorb more sunlight and start to thaw themselves, initiating a positive feedback loop where once a permafrost layer has thawed more than usual, it is much more likely to continue doing so in subsequent years.
“For example, higher surface temperature might cause the snow that's covering the upper permafrost layers to melt. And without the snow to reflect the Sun's toasty light back into space, the darker, newly-exposed layers would absorb more light and start to thaw themselves. And once a layer of permafrost has done a bit more thawing than usual, it's much more likely to continue doing so in subsequent years.”
Warmer temperatures wake up bacteria in the permafrost that decompose organic material and produce greenhouse gases as byproducts, and when the permafrost melts and collapses, these gases are released into the atmosphere, making things warm up even faster.
“These warmer temperatures also wake up bacteria in the ground that have been hanging out in what's basically a non-SciFi version of suspended animation. Then, they get to work decomposing organic material in the permafrost, producing greenhouse gasses as byproducts. And when the permafrost melts and collapses, those gasses are released into the atmosphere…making things warm up even faster.”
Paleontological remains discovered in the crater include ants, mushroom-inhabiting beetles, cave lions, wooly mammoths, and bison, demonstrating the fauna that inhabited the region throughout its geological history.
“They've even discovered animal remains…from the remnants of ants and mushroom-inhabiting beetles, to bones from much more charismatic fauna like cave lions, wooly mammoths, and bison.”
In 2018, one team discovered a roughly 40,000-year-old foal that was so well-preserved by the icy permafrost it still had hair and muscle.
“And in 2018, one team found a roughly 40,000-year old foal that was so well-preserved by the icy permafrost, it still had hair and muscle!”
Geologists hypothesize the permafrost layers were assembled over thousands of years as sand was blown over from a nearby floodplain, with alternating layers indicating the region went through cycles of freezing and relative warming during which meadows and coniferous forests grew.
“Geologists hypothesize that this cake was assembled over thousands of years. As the permafrost formed, sand was getting blown over from a nearby floodplain. But because of those alternating layers, we know this wasn't happening consistently. The region must have gone through cycles of freezing and relative warming…during which time you'd get stuff like meadows and coniferous forests growing.”
A different study found lemming remains in the crater that researchers estimated to be around 330,000 years old.
“Meanwhile, a different study found lemming remains that researchers estimated to be around 330,000 years old!”
The growing megaslump's runoff has made the river water unsuitable for drinking, affecting the residents in Batagay and clogging the waterway down to the sea it drains into.
“The runoff has also made the river water unsuitable for drinking, affecting the residents in Batagay and clogging the waterway down to the sea it drains into.”
The Institute of Applied Ecology of the North organizes scientific expeditions to the crater, with researchers needing to watch out for bears, mosquitos, and awakened ancient microorganisms in the region.
“The Institute of Applied Ecology of the North organizes scientific expeditions to the Crater. You just gotta watch out for all the animals in the region that are still very much alive…like bears, mosquitos, and all those ancient microorganisms that have just woken up!”
Satellite imagery shows the ravine gradually expanding over decades, taking on its stingray-slash-tadpole shape, and by 1991 had grown large enough for scientists to officially call it a megaslump.
“We actually have satellite images that show the ravine gradually expanding over the decades, taking on its stingray-slash-tadpole shape. And by 1991, it had grown so large that scientists could officially call it a megaslump.”
Melted permafrost typically forms massive puddles on the surface, but in the Batagay region where the terrain sits at different elevations with the tail section much lower, the water and eroded sediments drain into the nearest river, leaving a massive hole behind.
“Now, typically, melted permafrost will form massive puddles on the surface. But the region that Batagay Crater calls home isn't sitting at one single elevation. The "tail" part is much lower, so when all that ice melts, the water and eroded sediments can drain into the nearest river…leaving a massive hole behind.”
The Batagay Crater in northeast Siberia is approximately 88 hectares (about one square kilometer) as of 2023 and has been growing since it appeared in the 1960s, releasing greenhouse gases and pollutants into the local river.
“In northeast Siberia, there's a hole so massive it's been nicknamed the Doorway to the Underworld. As of 2023, it's about 88 hectares big, or a little less than one square kilometer. But here's the thing: since it appeared in the 1960s, that doorway has been growing, releasing tons of greenhouse gasses into the atmosphere and pollutants into the local river.”
The Batagay Crater is the world's largest retrogressive thaw megaslump, shaped like a stingray or tadpole, measuring 2,700 meters long and 990 meters at its widest point.
“The hole is vaguely shaped like a stingray or a tadpole, measuring 2700 meters long from head to tail, and 990 meters at its widest.”
The 55-meter tall sheer cliff at the head of the crater perfectly exposes the permafrost's layers, allowing geologists to directly sample and analyze the geological history.
“At the head of the proverbial stingray, there's a sheer cliff that's 55 meters tall, perfectly exposing the permafrost's layers.”
The Batagay Crater's terrain is composed of alternating layers of permafrost approximately 75 meters thick before the crater formed, consisting of bedrock at the base with alternating layers of icy and sandy material, with sandy layers containing woody material, peat, and biomass like pollen and insect remains.
“It's made of several layers of permafrost, which is like really wet land that's been continuously frozen for at least 2 years. And before the crater formed, those layers added up to something around 75 meters thick. There's a bedrock base at the bottom, and then alternating layers of stuff that's either a bit more icy or a bit more sandy. And the sandy layers have layers inside of them, too, made of woody material, peat, and other biomass like pollen and insect remains.”
Each year, the melted permafrost releases 4,000 to 5,000 tons of previously sequestered organic carbon.
“Each year, the melted permafrost also releases 4,000 to 5000 tons of previously sequestered organic carbon.”
Between 2019 and 2023, the edge of the crater's bowl retreated by 53 meters at an average rate of around 12 meters per year, demonstrating accelerating erosion.
“Like between 2019 and 2023, the edge of the crater's bowl retreated by 53 meters, at an average rate of around 12 meters per year.”
Since 1991, the Batagay Crater has lost an estimated 35 million cubic meters of matter, with two-thirds of that being meltwater and the remainder being sand and biomass that was layered throughout the permafrost.
“Since 1991, Batagay Crater has lost an estimated 35 million cubic meters of matter. Two-thirds of that has been meltwater, with the rest being a mix of sand and biomass that was layered throughout the permafrost.”
There is nothing we can immediately do to stop the Batagay Crater's growth, but it might stop expanding on its own within just a few decades because it is about to hit rock bottom—the crater is running out of permafrost to melt.
“Unfortunately, there is nothing we can immediately do to stop Batagay Crater's growth, but it might stop expanding on its own within just a few decades, because the situation is literally about to hit rock bottom. Below and at its sides, the crater is about to hit bedrock. It's running out of permafrost to melt.”