Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–2.5
Over the past few weeks, we have observed a relatively infrequent but continuous pattern of large avalanches or collapses failing on weak, faceted layers deeper in the snowpack. Persistent slab activity has been most problematic on wind-loaded terrain at higher elevations, though isolated instabilities exist below treeline. This avalanche problem has become unlikely to human trigger and will take just the right trigger point or a bigger load. It is still recommended to carefully assess the snowpack structure and give yourself a margin for error in handling this problem as there is a high degree of variability across the region and on different aspects. Some examples of recent persistent slab activity include a large natural in Conundrum Creek on 3/4, a very large skier-triggered avalanche near Aspen Highlands on 3/2, a remotely triggered avalanche near Friends Hut on 3/1, and a natural step-down avalanche near Coffee Pot Pass around 3/1.
A large persistent slab that ran over the past weekend. Outside of the forecast area near Ashcroft.