Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1.5–2.5
Weak layers are persisting in the snowpack beneath hard slabs 3-5 feet deep above 7500’ primarily on the north half of the compass. Triggering an avalanche is most likely where the overlying slab is thin and riders can impact these weak layers.
- The most obvious slopes will be rocky and wind affected terrain where thin trigger points exist.
- Gain more knowledge of a given slope by probing for snow depths before committing to consequential slopes. Feel for hard snow above weak snow. The weaker layer will be closer to the surface in shallower areas.
- Large triggers such as recent cornice falls indicate that these weak layers can still be reactive (see observation from the nearby Teton zone on Mary's Nipple).
The Wyoming Range harbors a weaker and shallower snowpack that is easier to impact these buried layers. The Snake and Salt River Ranges hold a deeper snowpack where this is less likely. However, thin areas where weak layers are more reactive can be found across the entire zone as seen on Sheep Pass on 2/17. Stick to lower angle and less consequential terrain to reduce the unpredictable nature of persistent slab avalanches.
(2/17/2024)
This rider trigger avalanche near Sheep Pass occurred on Saturday. The rider was caught but not buried.