Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 4
A widespread persistent weak layer (PWL) of faceted snow is now buried under feet of recent storm snow, creating dangerous avalanche conditions.
Strong winds and heavy snowfall have overloaded this weak layer, resulting in nearly 50 avalanches over the past three days, many of which were triggered naturally or remotely. With ongoing elevated winds and more overnight snowfall, avalanches on this PWL will only grow larger.
Avoid being on, underneath, or adjacent to slopes steeper than 30° in steepness. These slides can be triggered remotely, from a distance, or even from below.
Recent avalanches were reported from the Ant Knolls zone, including the Ant Knolls ridgeline, Ant Eater, Ant Hill, and other steep E-NE-E slopes above 9,000'. These avalanches likely occurred on the old faceted snow, with some possibly triggered by wind loading. This is an example of the type of avalanche we could see today.
Water percolating to the persistent weak layer at lower and mid elevations could trigger large avalanches, as seen Saturday with UDOT Provo reports of slides up to 2,400' wide and 2,000' vertical; while colder temperatures today reduce the risk, be alert to rapid warming, as dry avalanches could become wet and more dangerous, especially for ice climbers or those below steep slopes.