Glaciation refers to the process of the formation, advancement, and recession of glaciers. It is a natural phenomenon that has occurred multiple times throughout Earth's history, shaping the landscape and influencing the climate.
Glaciation is primarily caused by changes in the Earth's orbit and tilt, which affect the amount and distribution of solar energy received by the Earth's surface. These changes, known as Milankovitch cycles, can lead to periods of cooling and the accumulation of snow and ice, ultimately forming glaciers.
Glaciation has profound effects on the environment, including the carving of valleys and the formation of lakes, moraines, and other landforms. It also impacts global sea levels and can influence regional climates.
Understanding the process of glaciation and its impacts is essential for comprehending Earth's geological history and the factors that shape our planet's surface.