Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 3
Your main concern is triggering a large and unsurvivable hard slab avalanche that fails on weak faceted snow 2-5'+ deep. This weak faceted snow is a persistent weak layer that formed during our extended dry spell in December and was subsequently buried on January 4th. The initial indicator avalanche of this newly buried PWL was just two days later on the 6th in Main Porter Fork of MCC with an upward trend of avalanche activity with additional storms the following week. The world fell apart with an Extreme danger on Sunday Jan 14th with widespread avalanches on many aspects and elevations. Over time, this unstable combination has become more stubborn and yet they are no less deadly. (Again, it only takes a moment to spin through some photos of recent avalanches to see what I mean.) You can see the reported avalanche frequency for the SLC mountains below.
Beyond all the highlight reel avalanches are some booby-trap avalanches that have recently caught my eye from last Thursday and Friday. These PWL avalanches are well off the ridgelines and in the mid-elevation (some low elevation) bands but still large enough to catch, carry, and bury you. Don't let your guard down. Slope angle is slope angle. See this excellent example below from Mineral Fork from Friday - roughly 8800-9000'. Thinner snowpack areas, particularly outside of the Cottonwoods may be the most suspect. Remember avalanches may be triggered from a distance or below. A heat map of PWL avalanches for the SLC mtns from Jan 6th is below.