Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
A layer of lower density snow underlying firm wind deposits has created a difficult to manage slab problem on the upper slopes of Mt Hood. Although the reactivity continues to decrease, the consequences have not. Large slabs triggered in mitigation at Mt Hood Meadows both Monday and Tuesday were reactive to very small amounts of dynamite, suggesting that a rider could easily trigger them as well.
Given the size of the avalanche problem (potentially very large) above 6500 ft, it's unwise to commit to large wind-loaded slopes on the eastern half of the compass. Although reverse loading formed shallow deposits on W aspects on Tuesday, Monday's winds from the WSW formed the larger slabs that are most concerning. Below around 6500 ft, softer slabs should be healing more rapidly with another day of sunshine and mild temperatures. T
Given the strength of recent WSW winds,deposits may lurk near ridgelines, but also well below typical startzones around moraines and even low on canyon walls. Shooting cracks and hollow-feeling snow are both key indicators that the snow needs more time to settle before you engage with consequential terrain.