Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
Triggering a large, 1-2' thick avalanche is most likely on slopes with the following characteristics:
- Slopes steeper than about 35 degrees.
- Well-developed facets in the middle of the snowpack.
- Where wind has stiffened the snow in the upper part of the snowpack and/or formed hard drifts on the surface.
- Slopes that face W/NW-NW-N-NE-E-SE. These aspects are where the majority of our recent avalanche activity has occurred and harbors the ugliest underlying snowpack structure.
Skiers triggered 4 persistent slab avalanches near Galena Summit last weekend, including one that buried a skier to his waist. You can find details on these and other slides by visiting our Avalanche Database. SAC staff, local guides, and public observers continue to report extensive snowpack collapsing and poor stability test scores each day. You can check out what forecasters and others are seeing on our Observations page.
There's a real chance of remotely triggering slides—from areas below, above, and to the sides of steep slopes. Be aware of the terrain you are in and the terrain above you.
ADDITIONAL DISCUSSION - WIND SLABSLast night's snowfall may have formed fresh, sensitive drifts in exposed terrain. Though small in size, these slabs may be touchy and will add stress to the weak snow described above. Any small slides you trigger have the potential to "step-down", creating a much larger and more dangerous avalanche.
(12/27/2020) This avalanche failed at 9,500-9,900' on a E-NE facing slope at the head of Owl Creek in the Smoky Mountains. It appears to have released near the end of the storm on Saturday, 12/26.