Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 2–3
This zone has persistent weak layers buried 3-5 feet deep on most middle and upper elevation slopes (see snowpit). People often ask how these weak layers heal. There's no magical formula, but the most important factor is time. It's been a week or more since the snowpack has been significantly stressed by new snow, wind, or warming temperatures. Imagine how you'd feel after a week on the beach with no email, no texts, and no news. Given a week of relaxation, both you and the snowpack will feel better—but that doesn't mean your problems have miraculously disappeared forever.
As the likelihood of triggering an avalanche continues to decrease, it's important to understand where the chances remain the greatest. With deeply buried weak layers, it's important to avoid thinner areas where you are more likely to impact the weak layer:
- Wind-affected terrain: The wind can create thinner spots where the weak layer is closer to the surface. These are often connected to wind-loaded areas where there is more load on the weak layers.
- Steep, rocky slopes: Rocky or "alpine-like" terrain typically has shallow areas where your weight can more easily affect buried weak layers.
ADDITIONAL DISCUSSIONIn some upper elevation locations, yesterday's 1-2 inches of new snow was getting transported by gusty W to NW winds (see video). You may find thin, sensitive wind slabs (like these) today along higher ridgelines.