Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1.5–2.5
The weak snow buried near the base of this snowpack continues to be the primary avalanche concern in this zone. While encountering a wind slab (described below in Problem #2) is more likely, any wind slab you trigger has a chance of "stepping-down" to the weak snow near the ground.
The best way to assess this weak layer is to dig down, identify the layer, and perform stability tests before riding consequential terrain. It is worth carefully reading any recent observations over the past week in areas you frequent and grasp any trend with activity. You are most likely to encounter this problem on terrain that has the following characteristics:
- Located on the southern half of the compass at upper elevations (E-S-W): These areas remain shallower and weaker as any new slab builds.
- Wind-affected: Terrain where the wind has formed firm, cohesive slabs of snow.
- Steep: Terrain over 35 degrees in steepness.
Recent avalanche activity has occurred on this layer in areas with a thin, shallow snowpack such as the Wyoming Range, which bears similarities to Togwotee. (Dry Creek Lake, Hoback Peak).
(3/7/2023)
This avalanche occurred due to afternoon solar input at low elevations yesterday. Weak snowpacks remain widespread at Togwotee Pass, surrounding the town of Jackson, and low-elevation portions of the Greys. Any significant solar input or rain moving into the spring will likely cause an avalanche cycle in these areas.
Photo: Antonioli