Glide Cracks
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Temperatures are cooling, but the glide avalanche problem is not yet ready to be laid to rest. They happen when water lubricates steep areas which have a smooth bed surface (ground) such as bedrock or grass. They are very difficult to predict, but cracks, which usually form first, are a good indicator. Watch for deep cracks in the snow in steep areas, usually with ground visible at the bottom. Stay off large, unsupported slopes, or areas where you see these cracks and any slopes with similar characteristics nearby. These cracks might be hidden by a few inches of snow, but that does not mean that the snowpack is not wet underneath.
Glide cracks like this could turn into a glide avalanche.