Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
The persistent slab problem is most active in the upper meter of our snowpack. Faceted crusts on solar aspects, and buried near surface facets on shadier or wind-loaded aspects that formed during our recent dry periods are now buried beneath 1 to 2 feet of snow. These layers have been producing easy to moderate results in column tests, and in many cases they sit underneath a significant hard slab of snow, most notably in spots that see frequent wind-loading. This setup is now widespread in our snowpack, and it's where you're most likely to trigger an avalanche as a backcountry traveler. A persistent slab avalanche on this layer may break well above you and propagate widely across a slope. Watch for obvious signs of instability like shooting cracks and loud audible collapses in your travels.
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 but if you did find the right slab/weak layer combination they can produce a large avalanche failing on or near the ground. 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.
(3/9/2024)
Near surface facets from the February dry spell sit under a decent-sized slab (50cm+), such as this wind-loaded pit on an East aspect near treeline.
Photo: Charlie Harrison