Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
In the upper meter of our snowpack, we continue to observe crust/facet combos on solar aspects and buried near surface facets on shadier or wind-loaded aspects. These layers are buried beneath 1-2 feet of hard slab near the surface, and this setup is still pretty widespread in our area at all elevations. Because of the hard slab and additional crusts near the surface on solar aspects, you're unlikely to get any feedback from these persistent weak layers as you tour around. However, they have continued to produce easy to moderate results in column tests and short results in long PSTs. Any persistent slab avalanche of this variety has the potential to break well above you and propagate widely across a slope. Do your duty and dig around for these suspect weak layers before entering any consequential avalanche terrain, and use conservative terrain and group management tactics if you do decide to step onto steeper slopes.
Deeper down in the snowpack, depth hoar and the early January drought facet layer are still at play and continue to produce moderate to hard results in extended column tests where the snowpack is generally 1.5 m deep or less. These layers will be more difficult to impact and trigger today, but if you did find the right slab/weak layer combination they can produce a very large avalanche failing on or near the ground. Avalanche paths that ran already this winter are prime suspects for this particular setup. Avoid likely trigger points on the margins of the slab and near rock outcroppings as these will be the areas where you're more likely to impact these deeper buried weak layers. A probe pole can be a useful tool to identify snowpack depths on the slope you plan to play on.
(3/14/2024)
East Aspect near treeline. Near surface facets about 35-40cm deep failed on easy force in this spot.
Photo: Charlie Harrison