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Avalanche Types

Understanding the four main types of avalanches and how they form is fundamental to backcountry safety. Each type has different characteristics, triggers, and avoidance strategies.

Slab Avalanches

Slab Avalanches

Key Characteristics

  • Most dangerous and deadly type
  • Cohesive layer of snow breaks as a unit
  • Clear fracture line at the crown
  • Can release suddenly and propagate quickly
  • Often triggered by a person or external force

How It Forms

A cohesive slab of snow forms over a weak layer. When stress exceeds strength, the slab fractures and slides as a unit. The weak layer acts as a sliding surface.

Typical Conditions

  • Wind-loaded slopes
  • Recent storm snow
  • Temperature gradients creating weak layers
  • Buried surface hoar or faceted snow
  • Rain crust with new snow on top

Where They Occur

Slopes 30-45°, all aspects depending on problem type, commonly on lee slopes (downwind)

Loose Snow Avalanches

Loose Snow Avalanches

Key Characteristics

  • Start at a point and fan out downhill
  • No distinct fracture line
  • Snow lacks cohesion
  • Generally smaller and less dangerous than slabs
  • Can be dry or wet

How It Forms

Individual snow grains lose cohesion and begin sliding, entraining more snow as they descend. Forms a fan or inverted "V" shape.

Typical Conditions

  • Fresh, non-cohesive snow
  • Very cold, faceted snow (dry loose)
  • Warming or rain (wet loose)
  • Steep, smooth surfaces
  • Solar radiation on sun-exposed slopes

Where They Occur

Slopes steeper than 35°, often on very steep terrain (40°+), any aspect depending on trigger

Wet Avalanches

Wet Avalanches

Key Characteristics

  • Snow saturated with water
  • Heavy and slow-moving
  • Very dense debris
  • Can be loose or slab type
  • Predictable timing (diurnal warming)

How It Forms

Water infiltrates the snowpack, reducing strength and cohesion. Weight increases, bonds weaken, and snow loses ability to support itself.

Typical Conditions

  • Spring conditions with warming
  • Rain on snow events
  • Prolonged sunshine
  • Temperatures above freezing
  • Wet, heavy new snow

Where They Occur

Any slope angle steep enough to slide, often start spontaneously, sun-exposed and south-facing aspects most common

Glide Avalanches

Glide Avalanches

Key Characteristics

  • Entire snowpack slides on ground
  • Very slow to sudden release
  • Glide cracks visible days before
  • Full-depth avalanche
  • Unpredictable timing

How It Forms

Water lubricates the ground surface beneath the snowpack. Entire snow column slowly creeps downhill until it loses adhesion and releases as a full-depth avalanche.

Typical Conditions

  • Smooth ground surface (grass, rock slabs)
  • Water at snow-ground interface
  • Warm ground temperatures
  • Deep snowpack
  • Spring or warm winter periods

Where They Occur

Smooth, grassy slopes and rock slabs, any aspect, often below treeline, slopes 30-45°

Key Takeaways

Slab Avalanches = Most Deadly

Responsible for 90% of avalanche fatalities. Always take slab problems seriously and heed forecaster warnings.

Loose Snow = Common but Manageable

Generally smaller and more predictable. Watch for warming trends and avoid steep terrain when signs appear.

Wet Avalanches = Timing is Everything

Predictable based on temperature cycles. Early starts and knowing when to turn around are key.

Glide Avalanches = Unpredictable

Cannot be predicted or managed. Avoid all slopes with glide cracks—no exceptions.