Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2
The potential for humans to trigger a slab avalanche up to three in depth in steep north facing terrain continues to decrease. Some slopes that held snow from October are stable, and others remain suspect. This uncertainty is based on elevation, aspect, snow depth, the presence or absence of crusts and how the slope was loaded. In this situation, snow pits are useful for identifying snow structure. However, when evaluating the snowpack, remember that stability tests should be used to test for signs of instability, and the absence of significant test results should not be used as an excuse to ski or ride a slope.