Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–3
Weak layers that formed in early February have been waking up as the load over them increases. That trend could continue on Tuesday if sunshine helps consolidate low-density snow into a slab. In some areas, you could consider this a deep persistent problem. Elsewhere, these weak layers are shallow enough to label it as persistent. Regardless of its depth, this problem should be shaping your travel plans. Persistent weak layers don't heal quickly and will be with us for some time. You'll need to exercise patience by avoiding large open slopes where these unpredictable slides could fail. Just because a slope has tracks doesn't mean it's safe. All it takes is one person to find the "sweet spot" to trigger one of these beasts. Your best management tool will be to avoid large open slopes and their runouts where one of these wide, deep, and deadly avalanches could occur.
Natural and human-triggered slides have occurred on the Early February Crust (EFC) and other layers just above it near Crystal Mountain. Snowpack tests at White Pass and Paradise have resulted in sudden and clean breaks on these layers. In neighboring zones, avalanches on these interfaces have been triggered remotely and even resulted in a fatality on Friday in the nearby East South.
(3/4/2024)
A very large avalanche spotted near Sourdough Gap in the Crystal Backcountry. This likely occurred during the height of the storm on 2/29.
Photo: Andy Harrington