TubeReads

The Terrifying Real Science Of Avalanches

Every winter, thousands of skiers, snowboarders, and snowmobilers head into the backcountry—unaware that they are the ones most likely to trigger the avalanche that could kill them. 93% of fatal avalanches in the US are triggered by the victim or someone in their party. How can something so massive and destructive be set off by the weight of a single human? This video follows Whistler-Blackcomb ski patrollers as they deliberately trigger avalanches, revealing the hidden science of snow layers, weak zones, and the brutal physics that can bury a person in seconds.

Durée de la vidéo : 25:04·Publié 3 mai 2024·Langue de la vidéo : English
7–8 min de lecture·3,899 mots prononcésrésumé en 1,502 mots (3x)·

1

Points clés

1

93% of fatal avalanches in the US are triggered by the victim or someone in their party, making human judgment the most critical factor in backcountry safety.

2

Slab avalanches—the deadliest type—occur when a weak layer of faceted or surface hoar crystals fails beneath a cohesive slab, most commonly on slopes between 34 and 45 degrees where skiing conditions are best.

3

If buried in an avalanche, you have an 80% chance of survival if rescued within 10 minutes, but only 22% after 30 minutes, making speed of rescue the difference between life and death.

4

Ski resorts use explosive charges and artillery to deliberately trigger small avalanches before snow accumulates into deadly volumes, keeping skiers safe through proactive avalanche control.

5

Essential backcountry gear—beacon, probe, shovel, and avalanche airbag—can reduce fatality rates by nearly half, but the most important safety measure is checking forecasts and making smart terrain decisions.

En bref

Avalanches are not random acts of nature—they are predictable consequences of snowpack structure, temperature gradients, and human choices. The best way to survive an avalanche is not to be caught in one.


2

When Snow Becomes a Weapon

Avalanches killed thousands of WWI soldiers and claim 30 lives yearly in the US.

The deadliest snow avalanches in history occurred in December 1916 during World War I in the Dolomites mountain range of northern Italy. Over 12 meters of snow had fallen in the first week of December, and on the 13th, a single avalanche wiped out an Austrian barracks near Mount Marmolada, killing at least 275 people. But the true horror came next: both Italian and Austro-Hungarian forces realized they could weaponize the snow, firing artillery shells into mountains above enemy camps to deliberately trigger avalanches. Over the following days, between 2,000 and 10,000 soldiers died buried beneath the snow.

Today, most deadly avalanches aren't triggered by earthquakes or artillery. They're triggered by skiers, snowboarders, and snowmobilers recreating in the backcountry. Around 30 people die in avalanches each year in the US, plus an additional hundred in Europe. The terrifying truth: 93% of fatal avalanches in the US were triggered by the weight of the victim or someone in the victim's party. The question becomes: how could something so massive and destructive be triggered by the weight of just a single human?


3

Bruce Tremper's First Avalanche

A ski lift builder's cocky mistake led to a near-fatal avalanche encounter.

The first thing that happens when an avalanche brakes is it just starts moving and the first thing you do is kind of flop over on the snow. 'Cause you lose your balance. Like somebody pulls the rug out from underneath you and you fall uphill. And there I was just kinda laying in the snow, getting dragged down the mountain, you know, I was caught. I couldn't get out of it and luckily I was able to grab a small tree, but the snow was just beating me to death, and just about snapping off my neck as it's going by me on this tree.

Bruce Tremper


4

Avalanche Classification and Terrain

Avalanches range from person-sized to village-destroying and depend heavily on slope angle.

Avalanche Size Scale
1 to 5
Size 1 won't bury a person; size 5 involves 100,000+ cubic meters traveling many kilometers
Dangerous Slab Avalanche Zone
34–45 degrees
75% of dangerous slab avalanches occur in this slope range
Black Diamond Ski Run
~30 degrees
Double diamonds are around 40 degrees—prime avalanche terrain
Maximum Avalanche Speed
120 km/h
Slab avalanches can reach highway speeds in seconds

5

The Anatomy of a Slab Avalanche

🧊
Bed Surface
The strong, stable lower layer of the snowpack made of cohesive, rounded snow crystals that stick together like snowball snow.
⚠️
Weak Layer
Angular, faceted crystals or surface hoar that don't bond to each other, creating a failure plane where avalanches start.
🏔️
Slab
The cohesive top layer that breaks free as large chunks during an avalanche. Stiffer slabs propagate failure over greater distances, causing larger avalanches and more remote triggers.

6

How Weak Layers Form

Temperature gradients and surface condensation create the hidden danger zones in snow.

SURFACE HOAR
The Snow That Grows at Night
On cold, clear nights, the snow surface radiates heat and becomes colder than the air above it. Moisture in the warm air condenses directly onto the snow, forming delicate, angular crystals—the snow equivalent of dew. If buried by fresh snow before wind or sun can destroy them, these crystals become a particularly nasty weak layer that's perfect for triggering avalanches.
FACETS
When Temperature Gradients Reshape Snow
Facets form when there's a strong temperature gradient in the snowpack—more than one degree per 10 centimeters. Warmer snow near the ground sublimates into water vapor, rises through the snowpack, and refreezes on colder crystals above, forming angular facets. The bigger the temperature change, the faster snow crystals facet, and the faster they change, the more they promote instability and avalanche risk.

7

What Triggers an Avalanche

❄️
Storm Loading
The vast majority of avalanches occur during or right after a storm. The extra weight of new snow exerts additional load onto the snowpack, triggering weak layers to slide.
💨
Wind Slabs
Strong winds pick up and transport snow from open areas to sheltered zones. As snow accumulates, wind pressure compacts particles into dense, cohesive slabs that can be highly unstable over weak layers.
🪨
Cornices
Wind blows snow over ridges, creating overhanging masses weighing many tons. When cornices fall onto slopes below, they can trigger massive slab avalanches. Backcountry skiers test slope stability by dropping cornices onto terrain.

8

How Ski Resorts Control Avalanches

Explosive charges triggered before slopes open prevent snow buildup and keep skiers safe.

Before ski areas open each day, ski patrols perform avalanche control work. The fundamental strategy: trigger avalanches in a safe way before skiers arrive on or under those slopes, and do it often enough so snow doesn't build up into dangerous volumes. The most common method uses explosive charges with two-minute fuses, lit and detonated on slopes likely to produce avalanches. Sometimes charges are thrown from helicopters; often, patrollers deliver them on skis. Special trams even shuttle charges via carabiner to hard-to-access slopes.

As the charge detonates, the shockwave breaks the weak layer, releasing an avalanche. Avalanche control is also performed on mountain roads. For example, the Trans-Canada Highway through Rogers Pass—flanked by 3,000-meter peaks and literally passing Avalanche Mountain—is protected by Parks Canada and the Canadian Army, who fire artillery shells at 270 preset targets on nearby mountains. This releases small avalanches before they become big enough to damage the highway. Thanks to the diligent work of ski patrollers, deaths from avalanches in-bounds at resorts are very rare. Most avalanche injuries and deaths occur in the backcountry.


9

What It Feels Like to Be Caught

A producer's firsthand account of being swept down a mountain by snow.

To actually like feel the force of the avalanche on your body, like there's kind of nothing that can prepare you for that. Every time I hit the ground I would just like dig my hands in my feet in like try to like claw myself down onto the ground while also like trying to protect my head. I knew also like the moment the snow stopped, if I was still in the snow, I would be buried. I wouldn't be able to move, I would be counting on my buddy to find me and dig me out and save me.

Peter (Veritasium Producer)


10

Survival: The 15-Minute Window

Rescue time determines survival; buried victims have minutes before asphyxiation.

Survival Rate at 10 Minutes
80%
If friends find and dig you out in the first 10 minutes
Survival Rate at 15 Minutes
40%
Chance of survival drops by half after just five more minutes
Survival Rate at 30 Minutes
22%
After half an hour buried, odds of survival fall below one in four
Trauma-Related Fatalities
~25%
Deaths from hitting trees, rocks, or being pushed off cliffs; the rest are asphyxiation

11

Essential Backcountry Gear

📡
Avalanche Beacon
A transceiver operating at 457 kHz. In send mode, it broadcasts your location. If buried, your partners switch to search mode and follow the signal to find you. Invented in 1968, it's the foundation of companion rescue.
🔍
Probe & Shovel
Once the beacon narrows the search area, a collapsible probe pinpoints exact burial location. A shovel is essential to dig through avalanche debris, which sets like concrete after it stops moving.
🎒
Avalanche Airbag
Pull a cord to inflate an airbag (via compressed air or battery-powered fan), increasing buoyancy and reducing burial depth. If buried, the deflating airbag leaves a larger air pocket. Airbags decrease death rates by nearly half.

12

Why Buried Victims Can't Breathe

Friction melts snow during avalanches; it refreezes into an impermeable bubble around victims.

⚠️

Why Buried Victims Can't Breathe

During an avalanche, the snow mixes and friction heats it up, causing it to melt slightly. When the avalanche stops, it refreezes, setting like concrete—making it nearly impossible to dig yourself out. If your face is under the snow, there's a small air pocket to breathe, but the heat from your body and breath melts surrounding snow, which refreezes into an impermeable bubble. As you breathe, CO₂ concentration rises and oxygen drops until asphyxiation occurs.


13

Personnes

Derek Muller
Host / Narrator
host
Bruce Tremper
Avalanche Expert / Author
guest
Peter
Veritasium Producer
host
Aaron
Field Technician
guest

Glossaire
Surface HoarDelicate, angular ice crystals that grow on the snow surface through condensation on cold, clear nights, forming a weak avalanche layer if buried by fresh snow.
FacetsAngular snow crystals formed when strong temperature gradients cause sublimation and refreezing within the snowpack, creating weak layers prone to avalanche failure.
Wind SlabA dense, cohesive layer of snow deposited and compacted by wind in sheltered areas, often unstable when formed over weak layers.
CorniceAn overhanging mass of snow formed by wind blowing over a ridge; when it falls, it can trigger large avalanches on slopes below.

Avertissement : Ceci est un résumé généré par IA d'une vidéo YouTube à des fins éducatives et de référence. Il ne constitue pas un conseil en investissement, financier ou juridique. Vérifiez toujours les informations auprès des sources originales avant de prendre des décisions. TubeReads n'est pas affilié au créateur de contenu.