Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
The weak layer of snow that sits beneath the slab formed by our last signifcant snowfalls continues to be a problem. Though there are less reports of collapsing, the layer propagates cracks in the majority of test pits. Really obvious signs of unstable snow, like whoompfing, are occurring much less frequently but those test results and poor structure are enough. Don't let the less talkative snowpack lure you into stepping into consequential terrain where this avalanche dragon resides. The weak layer in play can be found by digging or probing and performing stability tests but these strategies will only confirm what you already know, the snowpack is shallow and weak. If you really want improve your odds of avoiding an avalanche, just assume the weak layer is there and stick to favorable terrain. Low slope angles under thirty degrees and slopes without rollovers are your friend. Steep, rocky and previously wind loaded terrain are not.