Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1
Blowing and drifting snow has caused the danger to increase. Unstable, fresh drifts have formed on the leeward sides of ridge crests and terrain features. Drifts are recognizable by their smooth, rounded appearance and cracking is a sign of instability. Fresh drifts have also added more stress to the buried persistent weak layer on northerly facing slopes increasing the odds for a deeper and more dangerous avalanche.