Glatiation is water slowly turning into ice, or a glacier.
Glaciation on interior plains can create unique landforms like drumlins, eskers, and outwash plains. The movement of glaciers can shape the landscape by depositing sediment and carving out valleys. Glaciation also leads to the formation of lakes and wetlands in the region.
Glaciation
Terminal moraine is not a characteristic of continental glaciation. Terminal moraines are formed at the furthest extent of a glacier, marking the point where it stopped advancing.
sand and gravel deposits
The presence of large moraines (deposits of glacial till), erratic rocks (boulders carried by glaciers), and drumlins (elongated hills formed by glacial action) would be more likely in a region of continental glaciation compared to a region of valley glaciation. The larger scale and extensive coverage of ice in continental glaciation are responsible for shaping the landscape in these ways.
Glaciation
Precipitation is rain, sleet,hail,snow,etc. and glaciation is the state of being covered in ice masses and snow basically
The presence of large ice sheets covering extensive land areas would be likely in a region of continental glaciation. This type of glaciation is characterized by vast ice sheets that spread over entire continents, unlike valley glaciation which occurs in mountain valleys and is more localized in scope.
The movement of compacted snow across an area!
Glaciation occurs when snow accumulates over time and compresses into ice. This ice then flows downhill under its weight, forming glaciers. Glaciers erode the land, carving out valleys and shaping the landscape through processes like plucking and abrasion.
Glaciation on interior plains can create unique landforms like drumlins, eskers, and outwash plains. The movement of glaciers can shape the landscape by depositing sediment and carving out valleys. Glaciation also leads to the formation of lakes and wetlands in the region.
Ice age.
oxbow lake
E.t. Phone home
Glaciation
Terminal moraine is not a characteristic of continental glaciation. Terminal moraines are formed at the furthest extent of a glacier, marking the point where it stopped advancing.
The Great lakes went through glaciation many thousands of years ago.