Types of Avalanches
Learning Goal 7j: Define an avalanche, and list and describe
types of avalanches.
What is an avalanche?
An avalanche can be simply defined as a
mass of snow that moves quickly down a mountain. There are two
main types: loose-snow (or sluff)
avalanches and slab avalanches.
An avalanche starts when a layer in the snowpack becomes
overloaded and fails. The two typical ingredients are: (1) a
pre-existing weak layer, and (2) a trigger. The trigger can be natural
(like new snowfall, new wind-deposited snow, or a rapid temperature
change), or human (a skier/snowboarder/snowmobiler adding weight). In
most slides where a person is caught or killed, they or someone
in their party are the trigger.
Loose-snow avalanches
Loose-snow avalanches, also called sluffs, are made up of
surface and/or near-surface snow that is not well-bonded. They begin at
a single point, gathering more loosely-bonded snow crystals from the
surface of the snowpack as they descend, gradually fanning out. After
the fact, you can recognize them by their inverted "V" pattern,
starting from a point and spreading out downhill.
Fig. 7j.1 - Loose snow avalanche or sluff.
Fig. 7j.2 - Loose snow avalanche or sluff.
This type of avalanche does not usually do any major structural
damage, or bury people, although it is possible for them to. More
often, they will knock a person off their feet and carry them downhill.
This can be deadly if it carries them into trees, over a cliff, or into
a terrain trap. Terrain traps are typically small gullies. Even
a small avalanche can quickly fill the small gully, burying you a
couple of metres under the snow in the gully bottom.
When skiing steep faces with loose snow, it's important to
practice "sluff management". To do this a skier skis down the "fall
line" (directly downhill) for a short distance and then shifts over
laterally on the face, and continues to ski fall line there. The sluff
from their original fall line continues down the face next to them, but
at a comfortable distance. Check out this clip on sluff
management from legendary snowboarder Jeremy Jones.
Fig. 7j.3 - Dry sluffs triggered by skiers on the
ridgeline. Steep Creek, BC. (Credit: West)
Further, if the snow has high liquid water content, it is more
likely to be swept along, and the avalanche has more mass. This is a wet
sluff avalanche and is often caused by significant snowmelt
from strong solar radiation, or by significant rainfall on the
snowpack. Wet sluffs are more common in springtime and in maritime snow
climates, where mild temperatures and rain-on-snow events happen more
often.
Fig. 7j.4 - A sluff near Broads Fork Twin Peaks,
Utah, USA. This dry sluff was fairly large and ran a long distance. It
buried our skin track from the way up. (Credit: West)
Fig. 7j.5 - A skier descends next to an old wet
sluff in the Mount Baker backcountry, Washington, USA. This sluff ran
during the heat of the afternoon on the previous day. It's likely that
later in the day, this slope would have once again been unsafe to ski.
(Credit: West)
Slab avalanches
A slab avalanche occurs when a layer somewhere beneath the
surface layer fails, and the cohesive layer(s) above it fracture into a
block (or blocks) and slide downhill (see Fig. 7j.6). A slab can
propagate for 10s or sometimes even 1000s of metres. Since slab
avalanches are typically larger than sluff avalanches, they tend to be
more destructive and more likely to bury a person. Slabs that form due
to high wind speeds in new snow are referred to as wind slabs.
Fig. 7j.6 Slab avalanche.
Slabs generally fall into two categories. Hard slabs are a
result of high density, well-bonded snow (sometimes formed by high
winds). They remain hard and cohesive blocks as they slide. Soft
slabs are comprised of lower-density snow that has more bonding
than newly-fallen, non-wind affected snow. Often, snow becomes bonded
well enough to form a soft slab after about two days on the ground. The
fracture is less likely to propagate as far in softer slabs, usually
resulting in a smaller avalanche. The blocks also tend to break up more
as they slide down the slope.
Fig. 7j.7 - Hard slab avalanche.
Fig. 7j.8 - Soft slab avalanche.
A less common category of slab avalanche is a wet slab.
These are typically a springtime phenomenon. The slab release results
from meltwater or rain percolating through the snowpack, and a
pre-existing weak layer becomes wet enough that its bonds lose strength
and fail. Wet slabs most often occur in the springtime when the
snowpack experiences, for the first time all season, several nights in
a row above freezing temperatures. Wet sluffs can be a warning sign,
indicating that a slope may be primed for a wet slab release.
Here's a summary table of the types of avalanches and their
characteristics:
Fig 7j.9 - Summary table of avalanche types (row
headers) and their characteristics (column headers). (Credit: West and
Howard).
Keywords: avalanche, hard slab,
loose-snow
avalanche, slab avalanche, sluff, soft slab, terrain trap, wet slab,
wet sluff, wind slab
Figure Credits
Howard: Rosie Howard
West: Greg West
Stull: Roland Stull
COMET/UCAR: The source of this material is the
COMET® Website at http://meted.ucar.edu/ of the University Corporation
for Atmospheric Research (UCAR), sponsored in part through cooperative
agreement(s) with the National Oceanic and Atmospheric Administration
(NOAA), U.S. Department of Commerce (DOC). ©1997-2016 University
Corporation for Atmospheric Research. All Rights Reserved.
NOAA: www.nws.noaa.gov
Google: Map data (c) 2016 Google
Wagner: Wendy Wagner, Chugach National Forest
Avalanche Information Centre