calving
When a piece of a glacier breaks off, it is called calving. This can result in the formation of icebergs.
The process of dissolving by breaking into smaller pieces is called dissolution. This is the process through which a solute makes a solution by breaking the solvent.
This process is called dissociation.
The process of a glacier picking up rocks and transporting them is called "glacial entrainment" or "glacial plucking." When a glacier moves over bedrock, it can freeze onto and pluck rocks from the surface, incorporating them into the ice. These rocks can then be transported and eventually deposited as the glacier flows and melts.
It's called floating the teeth.
The answer is a term called, Glacial Calving
Glacial inlet is called a fiord.
Post-glacial rebound (sometimes called continental rebound, glacial isostasy, glacial isostatic adjustment) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostasy.
Icebergs change size and shape constantly. When a fissure or crack develops and a portion breaks off it is called a floe. Changes in icebergs are determined by climate, pressure, force and temperature.
The process of breaking down complex food material and converting it into simple organic form is called digestion.
Glacial valleys can be straightened through a process called glaciation. As glaciers move down valleys, they can reshape them by eroding and bulldozing material, creating straighter and smoother profiles. This process is known as glacial erosion and can result in the formation of U-shaped valleys.
weathering