Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 3
Over the last two days many human triggered and natural avalanches were observed in the Central Wasatch, which has a similar snowpack. Most of these avalanches were triggered remotely, failing on the weak faceted snow and some were quite large, up to 2' deep and a few hundred feet wide.
Weak faceted snow from storms in early and mid-November makes up the base of our snowpack on most aspects at the mid and upper elevations. This layer will eventually begin to gain strength and heal; however, over the past few days, we quickly added around a foot of snow (or more), an inch of water, and continue to add strong winds at the mid and upper elevations. With this much weight and stress on this layer, as well as obvious signs of weakness like avalanches, this layer will not be trusted for the foreseeable future.
In this video Greg talks about the current snowpack in the Ogden area, find his full James Peak observation HERE.
Today, you are very likely to trigger an avalanche in terrain steeper than 30° that has the persistent weak layer of faceted snow buried underneath the storm snow. These avalanches can be triggered remotely and from below.