The formation you're referring to is called "till," which is a type of unsorted glacial sediment. As glaciers advance, they pick up and carry various materials, including rocks and soil, which become embedded in the ice. When the glacier melts or retreats, this material is deposited as till, and its abrasive nature can shape the landscape, creating features like moraines and outwash plains.
Glacial till is unsorted sediment deposited directly by glacial ice.
When a glacier deposits a rock with a different material composition than the surrounding formation, it is called "glacial erratic." These boulders are transported over long distances by the moving ice and can originate from vastly different geological regions. Their presence indicates the glacier's path and can provide insights into past glacial movements and the geological history of the area. Glacial erratics serve as important markers in understanding both glacial dynamics and the landscape evolution.
The debris of boulders and coarse material carried by glaciers is known as moraine. Moraines can be found at the edge, sides, and base of glaciers and are deposited as the glacier moves and melts. They can vary in size and shape depending on the glacier's movement and the type of material being transported.
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.
The rock is called a glacial erratic when it is left behind by a glacier, and is of a completely different material composition than the rocks on which it was deposited.
Material (such as rock) which is carried by a glacier.
Glacial drift
This is known as glacial till.
Glacial polishing is the process by which a glacier smooths and polishes a bedrock surface as it moves over it, causing striations and a shiny, polished appearance. This process is primarily caused by the abrasive action of rocks and sediments carried by the glacier as it moves.
The unsorted rock material deposited by ice when it melts is called glacial till. Glacial till can vary in size from clay to boulders and is typically a mixture of rock types that were picked up and carried by the moving glacier.
The glacier abrades the bedrock and the material is carried by ice. The groove is scoured in the bedrock by the boulders carried at the bottom of the ice. Grooves have various sizes.
Glacial drift refers to the material, such as rocks, sand, and clay, that is carried and deposited by glaciers as they move across the land. It includes both till, which is material directly deposited by the glacier, and stratified drift, which is material sorted and deposited by meltwater from the glacier. Glacial drift plays a crucial role in shaping the landscape and can be used by geologists to understand past glacial activity.
Glacial till is unsorted sediment deposited directly by glacial ice.
Glacial deposition is the process by which glaciers transport and deposit sediments, rocks, and other materials as they move. One example of glacial deposition is the formation of moraines, which are long ridges of material left behind by a glacier as it retreats.
Glacial drift is material that has been eroded, transported, and deposited by glaciers. It includes a mix of rock fragments, sediments, and debris that are carried along by ice and then left behind as the glacier melts or retreats. Glacial drift can vary in size and composition, depending on the location and movement of the glaciers.
Glacial sediments are typically unsorted, meaning they contain a wide range of particle sizes. They often show distinct layering or banding due to the way glaciers move and deposit material. These sediments may also contain a mix of rock types and sizes due to the abrasive nature of glacial ice grinding against the underlying bedrock.
Glacial Drift