New research has detailed the rate at which Siberia's massive Batagaika crater is devouring the surface of the Earth, expanding at a rate of 35 million cubic feet each year. Currently, it measures around 1 km (0.6 mi) long and 800 m (0.5 mi) across at its widest point. And it's speeding up.
Batagaika crater, located in the Chersky Range in northeastern Siberia, is not actually a crater but a thermokarst depression – a kind of sinkhole or 'mega-slump' driven by the collapse and fracturing of land due to permafrost loss. It was only discovered in 1991, after this underground opening split further and took with it a large section of hillside. In the video below, you can see its growth from discovery to 2007.
Permafrost, despite its name, is not actually permanent; it's essentially ground that's remained at 32°F (0°C) or colder for more than two years. A quarter of the Northern Hemisphere's land surface is made up of this rock-hard frozen dirt that can vary between a a few feet deep to almost a mile.
Its rapid expansion is now fueled by warming air temperatures, which has set off a positive feedback loop that's unlikely to slow down as long as there's ice to thaw. When the permafrost layer degrades, or melts, it goes from concrete consistency to a muddy mass, which is unable to support the vegetation on the surface. As the edges of the expanse collapse into it, the ground loses the canopies of trees shielding it from the sun (and heat).
At this point, newly-exposed organic matter, no longer preserved in ice, breaks down and releases carbon into the atmosphere to further fuel atmospheric warming. This, of course, results in increasingly more permafrost loss. As for the ancient bugs, we don't know whether they're equipped to survive for long when exposed to the Earth's atmosphere – but nor do we know if our modern biology and medicine is equipped to deal with novel viruses returning from 50,000 years of dormancy.
The dramatic Batagaika crater formation – which has earned it the nicknames of 'gateway to the underworld' and 'gateway to Hell' – has steep cliff-like edges revealing permafrost estimated to have been frozen for 650,000 years. It's currently around 50 m (164 ft) deep, with areas dropping down 100 meters (328 feet).
