Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Par for the course at Togwotee, the snowpack at middle and upper elevations is plagued by layers of weak snow, primarily on the northern half of the compass. The layers most likely to produce large avalanches in this zone are 1-3+ feet deep (dependent on aspect due to variability in snow depths) and consist of well-developed sugary, faceted snow. These can be pretty easy to feel on a sled, so if you trench your track into weak snow, take a minute to look at the structure of what you are riding and where that problem snow can be found on the problem diagram above. If you're finding this snow, it's best to steer clear of any steep slopes, even if these may appear unsuspectingly small, like the steep creeksides and gullies that are common around Togwotee.