Glaciers form in areas where snowfall exceeds snowmelt over many years, causing the accumulation of compacted snow and ice. Over time, the weight of the overlying snow compresses the lower layers into ice. This process, known as "glaciation," leads to the formation of a glacier.
Glaciers move due to the force of gravity and the gradual deformation of the ice. The process of movement, or "flow," occurs as the ice at the base of the glacier melts and refreezes, allowing the glacier to slide slowly downhill. This movement results in the characteristic "creep" of glaciers, which can range from a few centimeters to several meters per day.
Glaciers are powerful agents of erosion, capable of carving deep valleys, fjords, and cirques. The movement of glaciers scours the underlying bedrock, plucking and grinding rocks as they advance. This process results in the formation of features such as glacial valleys, roche moutonnée, and glacial erratics.
As glaciers move, they carry sediments and rock debris, which can be deposited as the ice melts. This process creates landforms such as moraines, drumlins, and eskers. The deposition of glacial sediments also influences the formation of fertile soils and contributes to the shaping of landscapes in glaciated regions.
Glacial activity has a profound impact on the environment, influencing factors such as climate, hydrology, and biodiversity. The melting of glaciers contributes to sea-level rise, while glacial meltwater serves as a vital freshwater resource for many regions. Additionally, the unique habitats created by glacial landscapes support diverse ecosystems and species.