Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 2
The base of the snowpack consists of a persistent weak layer of loose faceted (sugary) snow. A number of layers have been added on top of the weak snow. Imagine a building with a weak foundation but we keep adding additional floors on top - eventually the whole structure will collapse. Every slope has the weak foundation. What is different is how many floors are on top of it.
There have been a number of natural and human triggered avalanches because the weak loose snow collapses. This situation is going to continue for the foreseeable future. This is why these loose faceted crystals are known as a Persistent Weak Layer. The problem can persist for a long time.
What's tricky - the first person to ride on or even near a slope may not trigger it. Instead, it may be the 2nd, 3rd, or even 10th person on a slope who triggers it. Seeing tracks on slope doesn't mean it's safe. Also, typical with this buried faceted snow, a person can trigger avalanches from a distance.