Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Several weak layers exist within the upper snowpack that could fail and produce large avalanches Tuesday. As these layers gain strength and triggering a slide becomes more difficult, turn your attention to features where you might be more likely to cause a slide. Steep convexities, rocky and complex terrain, and unsupported slopes could produce large avalanches.
Over the last several days, multiple storms, fluctuating snow levels, and various types of precipitation created a layered snowpack. Unfortunately, the structure may change significantly with elevation, aspect, and proximity to the Pass with its cool easterly flow. As a result, don’t expect observations from one location or elevation to represent another. You’ll need to constantly look and check. Because of the strength and depth of some layers, small test slopes may not give you the information you need. Instead, you’ll want to dig with your hand or shovel and feel for strong (slab) over weak (weak layer). If you find a layer that fails easily steer around nearby slopes greater than 35 degrees to avoid triggering avalanches.
(12/19/2021)
Using simple hand pits while you travel is a quick way to gain some information about slab potential and the depth of potential weak layers in the upper snowpack.
Photo: Dallas Glass