Deep Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1.5–3
Weak layers of sugary facets exist in the middle of the snowpack and near the ground on most slopes. Avalanches involving these layers will be 2-3 feet deep and up to 5 feet deep on heavily wind-affected slopes. Triggering one of these dangerous avalanches is possible on very steep slopes over 35 degrees. Signs of instability such as cracking, collapsing, or recent avalanches may not be present before triggering a large avalanche capable of propagating long distances. Multiple tracks on a slope do not indicate stability with this problem type. Suspect terrain includes very steep, rocky, and/or wind-affected slopes where thin spots exist, making it possible for humans to impact buried weak layers.
Several days of above-freezing temperatures and a weak overnight freeze could increase the likelihood of triggering a persistent slab avalanche. Surface slabs could step down to deeper, weaker layers, resulting in a larger avalanche than expected.
The last human triggered persistent slab avalanche occurred on March 2nd in terrain similar to this.
Photo: Dakota Richardson