Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
Wind drifts remain the primary concern in the Provo mountains. They have becoming increasingly stubborn, but not dormant. They are more prominent in the upper elevations but also noted to the lee of exposed mid-elevation ridgelines. They'll be more prominently found on steep north to east to south facing terrain; even cross loaded on some southwest facing slopes. Human triggered avalanches are possible.