Glaciation refers to the process of the formation, advancement, and recession of glaciers. It is a key geological process that has shaped the Earth's surface over millions of years. Glaciers are large masses of ice that move slowly over land, carving out valleys and shaping mountains.
Glaciation is primarily caused by changes in the Earth's climate. Factors such as variations in the Earth's orbit, tilt, and precession (collectively known as Milankovitch cycles), as well as changes in atmospheric composition, can lead to periods of global cooling. This cooling results in the formation of glaciers in high-latitude and high-altitude regions.
Glaciation has a profound impact on the Earth's landscape. It can result in the formation of characteristic landforms such as U-shaped valleys, moraines, and drumlins. Glacial erosion and deposition also play a significant role in shaping the topography of regions affected by glaciation.
Here are some key topics to focus on when studying glaciation: