Snow Pack Stability

Snow pack stability refers to how securely snow layers are held together in the snow cover on a mountain or slope. It depends on factors like snow type, temperature, and weather conditions. When the snow layers bond well, the snow is stable and less likely to slide or cause avalanches. Conversely, if layers are weak or there are hidden weak spots, the snow can suddenly shift and trigger an avalanche. Assessing snow pack stability involves examining snow conditions, looking for signs of weak layers, and understanding weather influences to reduce the risk of snow sliding unexpectedly.