Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–2.5
Recent snow and strong wind have loaded slopes and produced slabs on top of deeper buried weak layers. In shallow snowpacks (<1.5m) before this storm, depth hoar, the early January facet layer, and faceted crusts continued to remain weak and slow to heal. These weak layers had been mainly lying dormant during the latest two-week dry period but could become more reactive with this latest load and slab formation. It will most likely take you finding a shallow spot on the slope near a likely trigger point on the margins of the slab or near rock outcroppings to trigger a persistent slab avalanche or triggering a wind slab on the surface that then steps down into deeper weak layers. These avalanches could be very large running well into the flats below and most likely not survivable. A probe pole can be a useful tool to measure snowpack depths on the slope you plan to play on.
This is an annotated snowpit from a NNE aspect near treeline that is 140cm deep. In places where the snowpack remains under 1.5 m deeper persistent weak layers have been slow to heal and continue to remain reactive in long column tests. These shallow spots on the slope are also where you're more likely to impact the deeper buried weak layers.
(2/28/2024) Photo: Andy Bond