What is a glacial collapse? How collapsing ice can trigger deadly floods, landslides and tsunamis

A glacial collapse occurs when a large section of a glacier suddenly breaks apart, falls or slides downslope.

THE TAKEAWAY

  • More than 157 people were killed and at least 400 are missing after a glacial collapse in Nepal.
  • A similar event occurred last year when an avalanche of rocks and ice from the Birch Glacier in southwestern Switzerland.
  • It also happened in Alaska when a landslide sent debris into the water below, unleashing a massive wave.

More than 157 people were killed and at least 400 are missing, including nearly 50 American tourists, after a glacial collapse triggered deadly flash flooding and landslides in Nepal’s Himalayan region.

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At approximately 8:30 a.m. local time Tuesday (around 10:45 p.m. ET Monday), catastrophic flooding swept through the Bhote Koshi River, destroying buildings and damaging roads, bridges, electricity infrastructure and communications.

According to the U.S. Geological Survey (USGS), the event was initially reported as an earthquake. However, after additional analysis, the USGS determined that the seismic energy was generated by a landslide.

"Additional analysis of long period seismic waves indicate that the seismic energy was instead generated by a landslide," the USGS said. "The shaking caused by the landslide was equal to a magnitude 5.2 earthquake."

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A glacial collapse occurs when a large section of a glacier suddenly breaks apart, falls or slides downslope. Several factors can contribute to a collapse, including melting ice, cracks within the glacier and unstable terrain, according to the National Oceanic and Atmospheric Administration (NOAA).

Events involving collapsing ice, rock and debris can have devastating consequences in mountain regions.

A similar event occurred last year when an avalanche of rocks and ice from the Birch Glacier in southwestern Switzerland barreled into a valley below, nearly burying the village of Blatten and damming the Lonza River.

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According to NASA, the event occurred after rocks from a crumbling mountain peak accumulated on the glacier. The debris then descended the southern side of the valley from a peak called Kleiner Nesthorn toward Blatten.

Everyone in the village was evacuated, but one man died after remaining outside the evacuation zone.

"In particular cases where we know there is a danger, you can set up early warning systems," University of Dundee geoscientist Dr. Simon Cook told FOX Weather. "So that involves, for example, the use of time-lapse cameras. You might see seismometers. You need to have a system by which people can get warnings about those things through a cellphone. And, of course, we know in remote mountain regions there isn’t always cellphone coverage."

In another example, a landslide from a mountainside above a softening glacier in Alaska’s Tracy Arm fjord sent debris into the water below, unleashing a massive wave that reached more than 1,500 feet high.

The 481-meter (1,578-foot) megatsunami tore through the scenic Alaskan waterway about 45 miles south of Juneau.

The debris fall triggered what researchers described as the second-largest tsunami wave ever recorded.

As climate change continues to reshape environments, scientists are monitoring glaciers, slopes and surrounding terrain for signs of instability. 

While early warning systems can help communities prepare, experts say the remote locations can make detecting and responding to sudden collapses challenging.

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