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A late winter avalanche in Gran Paradiso National Park, Valle d'Aosta, Italy.
P H OTO G R A P H BY S T E FA N O U N T E RT H I N E R , N AT G E O I M AG E C O L L E C T I O N

REFERENCE

Avalanches, explained
Avalanches are masses of snow, ice, and rocks that fall rapidly down a
mountainside. They can be deadly.

B Y J E N N Y H O WA R D

P U B L I S H E D J U LY 1 9, 2 0 1 9 • 8 M I N R E A D

Falling masses of snow and ice, avalanches pose a threat to anyone on

snowy mountainsides. Beautiful to witness from afar, they can be deadly
because of their intensity and seeming unpredictability.

Humans trigger 90 percent of avalanche disasters, with as many as 40

deaths in North America each year. Most are climbers, skiers, and
snowmobilers. Learning about avalanches, and the conditions that cause
them, can help people recreate more safely in the backcountry.

Types of avalanches
The recipe for an avalanche may seem simple: a mountain slope and a
thick layer of snow. But Simon Trautman, an avalanche specialist at the
U.S. Forest Service’s National Avalanche Center and Northwest Avalanche
Center in Washington, says it’s actually a trifecta that causes avalanches:
terrain, snowpack, and weather conditions. Avalanches do occur naturally,
but when you add humans into the mix, they can be deadly, says
Trautman.

Avalanches come in many shapes and sizes. Many are small slides of
powdery snow that move as a formless mass downslope. Outdoor
recreationists often trigger these small “sluffs,” as well as more medium-
sized avalanches.

Disastrous avalanches occur when massive slabs of snow break loose from
a mountainside. The mass of snow shatters like broken glass as it races
downhill. These hazards can travel as fast as cars on a freeway, up to 100
miles per hour, says Trautman.

Snow slides can start on mountain slopes with at least a 30-degree incline,
but they occur most frequently on slopes of 35-50 degrees. Although
avalanches need a slope to start, large avalanches accelerate downhill with
sufficient momentum to cross flat terrain for short distances.

In some cases, a large chunk of ice or small glacier breaks off a

mountainside, gathering snow and momentum and rushing down in a
dangerous steamroll. One of the most deadly avalanches on Mount
Everest, which killed 16 Sherpas, occurred when an ice mass the weight of
657 buses plummeted down on top of hikers.

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2:55

AVA L A N C H E S 1 0 1
Learn the warning signs of an avalanche before it's triggered.

Features of avalanches
Avalanches contain three main features: the starting zone, the avalanche
track, and the runout zone. Avalanches launch from the starting zone.
That’s often the most unstable part of the stope, and generally higher on
the mountain.

Once the avalanche starts to slide, it continues down the avalanche track,
the natural path it follows downhill. After avalanches, large clearings or
missing chutes of trees provide clues to an avalanche’s trajectory.

The avalanche finally comes to a stop at the bottom of a slope, in the

runout zone, where the snow and debris pile up.

What conditions cause an avalanche?

Avalanches are most common during the winter, December to April in the
Northern Hemisphere, but they do occur year-round.

To get an avalanche, you need a surface bed of snow, a weaker layer that
can collapse, and an overlaying snow slab. The highest risk period is
during and immediately after a snow storm. Underlying snowpack,
overloaded by a quick deluge of snow, can cause a weak layer beneath the
slab to fracture naturally.

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Human-triggered avalanches start when somebody walks or rides over a

slab with an underlying weak layer. The weak layer collapses, causing the
overlaying mass of snow to fracture and start to slide. Earthquakes can
also trigger strong avalanches.

By digging a snow pit or profile, scientists can look at the composition of

different snow layers that formed during a season, sort of like looking at
the layers of a cake. The size and shape of the snowflakes in each layer
provide clues about the weather events that occurred: big dumps of snow,
drought, rain, a hard freeze, or loose, powdery snow. Larger, looser snow
crystals are weaker, because there are fewer points they can touch to
interact with the other snow layers. The interaction of the snow layers can
help predict the chances of an avalanche.

“Snow is an incredibly dynamic and complicated medium, which means

avalanches are the same,” says Trautman. He emphasizes that conditions
can change rapidly with the weather, and this can be deadly.

Slopes shaded from direct sun stay cooler, preventing bonding between
snow layers and leading to more avalanches in cold conditions. Conversely,
during the spring, sunny mountainsides have a higher risk for avalanches
because of rapid warming and melting. The number of “wet snow” slides
could increase in the future with climate change, experts warn.

Precipitation type and intensity, temperature, wind, slope steepness and

orientation (the direction it faces), terrain, vegetation, and general
snowpack conditions can influence whether and how snow moves down a
slope. Moving across the terrain, slight changes in slope or how the
mountainside is oriented towards the sun can create drastically different
conditions.

Take avalanche danger seriously

The Forest Service runs 14 backcountry avalanche centers in the United
States to provide information for people recreating in snowy wilderness
areas. Forecasters use four main elements to describe conditions, assign a
danger level, and help recreators make the best decisions in the
backcountry.

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Field teams at avalanche centers document the snowpack—the thickness

and type of snow layers—and combine those data with weather conditions
to estimate danger levels. The forecasts take into account the potential
type and size of an avalanche, the likelihood it will occur, and the location.

2:27

P R E V E N TAT I V E AVA L A N C H E
An officer supervises the use of a howitzer cannon to start controlled avalanches.

In some instances, forest rangers can blast cannons and other military
artillery at unstable snowpack to trigger avalanches in a safe and
controlled manner—when people aren’t present.

Before entering the backcountry, check online forecasts for the danger
level in that area. Each mountain range has unique snow properties and
therefore, avalanche risks, so checking your specific region is critical. New
Zealand, Canada, and Europe also maintain year-round forecasts of
avalanche danger for specific peaks and wilderness areas.

Experts recommend hiking and travelling earlier in the day. Weather

conditions can change rapidly, and warming during the day creates more
unstable snowpack with a higher risk for avalanches.

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Education and proper training on avalanches can help prepare you. Heed
all warnings and signs. Some accidents have been traced to people
avoiding warnings due to psychological traps, like desiring the ultimate ski
slope, untouched by humans.

Constant vigilance when you are outside can help avoid causing or getting
swept up in avalanches, but even trained experts can be become victims.
Be aware of the weather and terrain, and know your comfort level before
you embark on an adventure. (Read more about avalanche safety tips.)

If caught in an avalanche, try to get off the slab. In best case scenarios, this
is difficult. Skiers and snowboarders can head at a 45-degree angle
downhill to gather speed and veer left or right out of the slide path.
Snowmobilers can punch the throttle to power out of harm's way.

No escape? Reach for a tree. No tree? Swim hard. The human body is
denser than avalanche debris and will sink quickly. As the slide slows, clear
air space to breathe. Then punch a hand skyward.

Once the avalanche stops, it settles like concrete, making body movement
nearly impossible. Wait—and hope—for a rescue. (Read about rescue dogs,
trained to locate and dig out avalanche victims.)

“Learning about avalanches really helps people decide when and where,
and how to recreate,” said Trautman. “We shouldn’t all be terrified of this
stuff, but we should take it seriously. It’s supposed to be fun!”

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