Last week, North Korea announced that it will cease all nuclear testing and will shut down its main testing facility at Mount Mantap. Although some believe the decision came because of easing tensions between the country and the world, others think Mount Mantap may have come down with a bad case of "tired mountain syndrome."
But what exactly is tired mountain syndrome, and how does a mountain "catch" it?
It turns out that repeated nuclear blasts can weaken the rock around underground nuclear test sites, eventually making them unsafe or unusable — which might have happened with North Korea's preferred testing grounds. [North Korea: A Hermit Country from Above (Photos)]
In fact, the explosion registered as a magnitude-6.3 earthquake, and before-and-after satellite shots showed visible movement at Mount Mantap — a 7,200-foot-high (2,200 meters) mountain under which deeply buried tunnels house most of the tests. Some geologists think that the mountain is cracking under the pressure.
"You can take a piece of rock and set it on the ground, take a hammer, tap it; nothing will happen," said Dale Anderson, a seismologist at Los Alamos National Laboratory. You keep tapping it — and, say — the 21st time, "it will break and crack open."
When a nuclear explosion goes off inside a mountain, it breaks the surrounding rock, and the energy propagates out like a wave (imagine throwing a pebble into a lake). But as more explosions go off around the same — but not exact — spot, rocks that are farther away also begin to crumble under repeated stress.
"The accumulated effect of these explosions that weaken rocks and create that fracturing [farther away from the point of explosion] is what we call tired mountain syndrome," Anderson told Live Science.
Tired mountain syndrome can also stymie scientists trying to measure how strong an explosion is, he said. The propagating energy scatters around these fractured rocks before reaching the sensors, so the explosion registers as a lot weaker than it actually is, he added.
But this effect "has nothing to do with being able to use the facility," Anderson said.
In fact, a country can keep using the site but must adjust the mathematical equations it uses so that the final magnitude of the explosion takes tired mountain syndrome into account.
"Mother nature has already fractured the rock," Anderson said. "When an explosion goes off, sometimes damage [from it] will connect with natural fractures, and you can conceivably get a pathway up to the surface, and gases will seep out."
The process by which gas could be pulled up and through the rock is called barometric pumping.
A group of Chinese geologists said on Wednesday (April 25) that they believe the nuclear test site had collapsed and that Mount Mantap was in "fragile fragments," according to The Washington Post. But William Leith, the senior science adviser for earthquake and geologic hazards at the U.S. Geological Survey — who with one other scientist coined the term to describe a Soviet nuclear testing site in 2001— doesn't think it is.
In an interview with CBC Radio in October, when asked if the mountain in North Korea was tired, he said, "I would say, 'not very tired.' And that's because they've only had, as far as we know, six underground nuclear explosions, and there's a lot of mountain left there."
In comparison, he and his colleagues first used the term to describe Degelen Mountain in the former Soviet Union (now Kazakhstan), which was battered by more than 200 explosions.
North Korea's mountain may be tired — but whether it's completely exhausted is difficult to say.
Originally published on Live Science.