Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Observations indicate that day to day improvements in the deeper snowpack stability are occurring. No new post storm avalanche occurrences were reported yesterday. No additional reports of snowpack collapses or whumpfs were reported yesterday from newly traveled areas or from areas that were previously unstable. Snowpack tests suggest that the persistent weak layer of surface hoar (weak feathery snow crystals) and facets (weak sugary snow) at the base of 2 to 4 feet of recent storm snow is bonding into the snowpack and gaining strength. While the likelihood of triggering a large to very large persistent slab avalanche that fails several feet deep has decreased, it still remains possible today as the snowpack does not stabilize at the same rate in all locations.
If you are venturing into terrain where this avalanche problem could linger, choose routes that have options that allow you to divert to non-avalanche terrain if signs of instability such as collapsing or whumpfing are encountered. In between exposing only one person at a time to avalanche terrain, utilize robust safe zones for regrouping that will provide true protection in the event of a large and unexpected avalanche.
If you desire to minimize your chances of encountering this avalanche problem, travel on S-SW-W aspects or travel only on sub 30 degree angle slopes not connected to steeper terrain above or to the side.
(2/14/2025) Photo: Ming Poon
The reported persistent slab avalanches that were triggered post storm occurred in below treeline terrain. This avalanche was remotely triggered on 2/14 on a NE aspect. Hidden Peak, West Shore Tahoe area, CA