This document discusses avalanches and defines them as rapid flows of snow down sloping surfaces that are triggered in starting zones and form gravity currents. It describes how avalanches occur due to factors like temperature differences between snow layers, evaporation of lower layers, and loss of grip. The anatomy of an avalanche includes the starting zone where snow can fracture and slide, the track path down the slope, and the runout zone where snow comes to a stop. Formation involves terrain angle and slope, snowpack structure with weak layers below slabs, and weather conditions like temperature rises or storms. Types include loose snow, slab, powder, and wet snow avalanches. Effects range from positive like habitat to negative like damage and