Alpine Glaciers
Alpine Glaciers are large masses of ice that form in high mountain valleys, typically flowing slowly downhill due to the force of gravity. They are formed from the accumulation of snow over many years, which compacts into ice under the weight of additional snowfall. Alpine glaciers are important indicators of climate change, as their size and movement can be influenced by temperature and precipitation patterns. These glaciers are found in mountainous regions around the world and play a crucial role in regulating water flow in rivers and streams.