The color of a lake is influenced by a complex interaction of depth, light absorption, and the presence of organic or mineral materials. Pure, deep water appears blue because it absorbs longer wavelengths (reds) and scatters shorter blue wavelengths. However, many lakes appear green due to the presence of phytoplankton and algae, which contain chlorophyll. If a lake has a high concentration of Glacial Flour (fine rock particles from melting glaciers), it can appear a brilliant turquoise or "milky" blue, as these particles scatter light in a specific way. Conversely, "tea-colored" or brown lakes are often high in tannins from decaying vegetation in surrounding forests or bogs. In 2026, environmental scientists also monitor "turbidity"—the amount of suspended sediment—which can turn a lake brown or gray after heavy rainfall. Even the sky affects the color, as a lake's surface acts as a mirror, reflecting the blue of a clear day or the gray of an overcast afternoon.