Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 2–3
Weak facets and collapsible crusts are widespread on the northern half of the compass and on some sunnier aspects at high elevations. Slabs on top of these weak layers average 2 to 3 feet thick in wind-sheltered terrain. Slabs are thicker and harder in wind drifted terrain and can step down through older slabs to the ground. This problem is becoming more stubborn to triggers, often requiring a thin spot on the slope, such as near buried rocks, trees, or where slabs thin from wind effects. Avalanches can break widely across multiple terrain features and be remotely triggered from flat terrain near or below steep slopes without warning signs. The problem is less likely on southerly aspects due to recent melwater refreezing in the snowpack, and can be avoided on slope angles consistently less than about 30 degrees.
These destructive persistent slabs released on Wednesday 2/19. These exemplify the potential size avalanche you could trigger on large, drifted slopes.