Avalanche path | A terrain feature in which an avalanche occurs, this is normally split into the start zone, track and runout zone |
Avalanche terrain | Any terrain which has the potential to form or be part of a snow avalanche |
Bonding | Refers to a snowpack which has undergone some metamorphism and has many links between the individual snow grains, generally leading to a stronger “bonded” snowpack |
Cornice | An overhanging mass of wind sculpted snow projecting beyond the crest of a ridge |
Crust | A hard surface layer which can be formed by solar radiation, wind or rain which has the potential to cause instability when buried |
Destructive Scale of Avalanches | D1: Relatively harmless to people. Typical mass: less than 10 tons.
D2: Could bury, injure or kill a person. Typical mass: 100 tons. D3: Could bury and destroy a car or truck, destroy a wood frame house, or break a few trees. Typical mass: 1000 tons. D4: Could destroy a railway car, several buildings, or a substantial amount of forest. Typical mass: 10,000 tons. D5: Could gouge the landscape; the largest known avalanches. Typical mass: 100,000 tons. |
Freezing level | The elevation at which the air temperature is at 32° Fahrenheit or 0° Celsius |
Half (1/2) | Used with compass directions, e.g. “lee to the easterly half” refers to the aspects facing west from north through to south |
Instability | A weakness or lack of stability indicating that additional loads will result in a given probability of avalanche occurrence |
Lee (leeward) | The side of a mountain protected from the wind (where snow is deposited by the wind and loading occurs) |
Loose snow | A type of avalanche which originates at a point and spreads out as it descends (aka “sluff” or point release) |
Melt-freeze | A metamorphic process when snow changes from a solid to a liquid and back again and may result in the formation of a crust. |
Pockets | Small isolated terrain features |
Quarter (1/4) | Used with compass directions, e.g. “lee to the easterly quarter” refers to the aspects facing northwest through to southwest |
Runout zone | The area at the bottom of an avalanche path where an avalanche starts to decelerate and comes to rest; this is where the debris is located after an avalanche has occurred |
Safe travel technique | The use of appropriate terrain to move given the posted danger scale (e.g. stick to ridges and well away from runout zones, or slopes less than 30°) |
Shady aspect | The side of a mountain protected from the sun |
Slab | A cohesive layer of snow |
Sliding hazard | A hazard posed by very hard or icy conditions, also known as “slide-for-life conditions” |
Solar aspect | The side of a mountain exposed to the sun |
Start zone | The area at the top of an avalanche path in which unstable snow may fail; most commonly has an angle greater than 25° |
Terrain traps | Terrain features which in the event of an avalanche could compound the danger (e.g. gullies, depressions) |
Track | The area which connects the start zone and runout zone, which can be either confined or unconfined |
Unsupported slope | Slopes which are not supported by the terrain (e.g convex rollovers) |
Weak layer | A layer in the snowpack identified as a possible failure plane |
Wet snow | Snow with a water content greater than 3% and temperature of 32° fahrenheit or 0° Celsius |
Whumphing | The sounds associated with rapid settlement or collapse of the snowpack, when weighted |
Wind loading | The transport of snow by the wind causing additional build up of snow on lee terrain or in deposition areas |
Wind slab | A cohesive layer of snow caused by wind loading |
Windward | The side of a mountain exposed to wind (from which snow is transported to lee aspects or deposition areas) |