avalanche path

An avalanche path is the specific zone on a mountain slope where snow is most likely to slide down rapidly, often causing an avalanche. It is shaped by the terrain’s features—such as slope steepness, rock formations, and vegetation—that influence how snow accumulates and moves. Avalanche paths typically have a defined funnel-like shape, guiding snow downhill. Recognizing these paths is important for safety and hazard management, as they are areas where avalanches are most prone to occur. Proper assessment of avalanche paths helps in planning safe routes and implementing protective measures in mountainous regions.