Predicting avalanches based solely on the static data we acquired proves difficult as avalanches are a dynamic process which changes considerably over a small area. The maps we created can only be used as a tool to aide in a risk based decision making process, and not as a definitive avalanche predictor. This project was limited by a lack of resolution in the data. The majority of factors were based off of a 25m x 25m DEM, had a smaller resolution DEM been acquired more accurate results could have been produced. This is important as avalanches can be triggered by a single, concentrated failure which could not be represented on a resolution that large. This project can prove as a basis for future avalanche prediction maps, and can be slowly improved through the improvement in spatially represented weather data and the ease of access for high resolution spatial data.