Glaciers form through the accumulation of snow in mountainous areas. When snow falls during winter and does not melt during cold spring and summer months, it compacts into dense ice over many years under its own weight. Additional layers of snow become compressed into ice, which causes the air to be squeezed out, turning the glacier a blue color. The large mass of ice then flows down the mountain under its own weight, eroding the landscape through two main processes - plucking and abrasion. Plucking involves rocks becoming frozen to the base of the glacier and breaking away as it moves. Abrasion occurs as rocks and debris carried on the glacier's bottom scrape along the valley floor, slowly excavating and shaping the land over