Forecast for the Abajos Area Mountains
Friday morning, January 9, 2026
New snow and wind have increased the likelihood for human triggered avalanches. Avalanches involving fresh deposits of wind drifted snow as well as avalanches failing on a buried persistent weak layer of sugary, faceted snow are possible. Unstable slabs of wind drifted snow are likely to form on the leeward sides of ridge crests and terrain features such as gully walls and sub ridges. Suspect steep slopes that have more than about 8 inches of freshly deposited, wind drifted snow. Wind drifts are often recognizable by their smooth, rounded appearance and cracking is a sign of instability. A triggered wind slab avalanche may step down into deeper, weak layers in the snowpack. You are most likely to encounter this problem on steep, northerly facing slopes.