Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Thick slabs from recent snow and wind rest on top of weak faceted layers that formed prior to this latest storm making for a strong over weak snowpack. These faceted weak layers formed around crusts, sandwiched around slabs or in some cases consisted of the upper 20 cm of snow. A cohesive slab resting on top is giving us this strong over weak snowpack structure.
Pay attention to loud audible whumpfs and shooting cracks as these are indications of unstable snow. Avoid being on or connected to steep slopes above as it is possible to trigger an avalanche from below. These avalanches could be large enough to injure or bury you.
Recent natural avalanche on an east aspect on the Lake Fork ridgeline. These east and north aspects on the leeward sides of ridgelines have seen the greatest amount of snow transport where slabs could be 2 to 4 feet thick.