Glide Cracks
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
Limit your exposure to steep terrain and the lower angle slopes beneath them, especially where you see cracks or wrinkles in the snow that indicate where the entire snowpack is slipping on a smooth ground surface. These are the conditions when very large avalanches may occur. Blocks of melting snow clinging to rock faces are also a red flag.
After days of hot weather, we suspect most avalanches have already happened. However, glide activity lingers even as temperatures begin to cool, since water may still be percolating down through the snowpack. While many slopes have shed wet snow, natural loose snow avalanches can still be triggered by cornice fall or snow shedding from rocks and cliffs.
Example photo: Glide cracks and avalanches seen in the Del Campo area of the Mountain Loop Highway in a previous year. Don't travel beneath cracks like these. Photo: Irene Henninger