Deep Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 3
Unintentional human triggered avalanche activity continues to be a near daily occurrence in areas where persistent slabs exist. Yesterday's reported avalanche activity occurred on Andesite Ridge (Donner Summit area)(more info below in recent observations). Buried surface hoar is a persistent weak layer that remains unstable for prolonged periods of time. Open areas near treeline and below treeline on N-NE-E aspects hold the greatest concentration of buried surface hoar with 1 to 3 layers buried 2 to 3 feet deep. NW and SE aspects near treeline and below treeline hold isolated areas of buried surface hoar.
There are 8 different types of avalanche problems. Wind slabs are the common avalanche problem in the Sierra. Instability usually last for hours to days and wind slab location is very predictable. Persistent slabs focused on buried surface hoar layers are an entirely different problem with very different characteristics and predictability in terms of location and length of unstable time period. Travel in the backcountry requires a different approach when managing persistent slabs as opposed to managing wind slabs. With persistent slabs, anticipate the potential to trigger avalanches low on slopes, after slopes have been traveled by others, and in lower angle terrain in the 30 to 35 degree slope angle range. Communicate with your partners and adjust terrain selection and travel practices in accordance with the avalanche problem, not just based on the overall danger rating.