Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–2
Since 12/9, several northwest-to-southwest wind events formed slabs around a foot thick. These wind-drifted slabs are most commonly found at higher elevations below leeward ridgelines and rollovers on east and northeast-facing terrain. They can also be found around the northern half of the compass in a few concave terrain features that collect drifting snow, such as gullies. These slabs are often hard and difficult to manage, breaking unpredictably and with inconsistent feedback underfoot. Because many of them formed over weak, faceted snow, instabilities are slow to heal. Assess recent wind-loading patterns and consider avoiding previously wind-loaded terrain features, especially in high-consequence terrain.