An avalanche can be triggered by several factors, including heavy snowfall, rapid temperature changes, vibrations, or human activity. When a significant amount of new snow accumulates, it can destabilize the existing snowpack, increasing the risk of collapse. Additional factors, such as a sudden warm spell that causes melting or a skier’s weight on a steep slope, can lead to an avalanche release. Understanding these triggers is vital for avalanche safety and for developing effective monitoring and prediction strategies in mountainous regions prone to these natural hazards.