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 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.
Geographers conclude that moraines are indicators of past glacial activity. These ridgelike piles of rock and debris are formed from the accumulation of materials that glaciers have eroded and transported as they advance and retreat. The presence and characteristics of moraines can reveal information about the movement and size of glaciers, as well as the environmental conditions during the periods of glaciation.
There are several names: outwash is one and moraines are another. The outwash forms a flat area sometimes called outwash planes and the moraines are hilly.
Sediment found in glacial moraines is best described as unsorted and unstratified debris. This material is typically composed of a mixture of clay, silt, sand, gravel, and larger boulders that have been picked up and transported by the moving glacier. As glaciers advance and retreat, they deposit this sediment at their edges, resulting in the characteristic ridges and mounds known as moraines. The heterogeneous nature of the sediment reflects the varied geological sources from which it was eroded.
The furthest advance of the continental ice sheets during the Ice Age is marked by terminal moraines, which are ridges of debris deposited at the glacier's edge. These moraines indicate the maximum extent of glacial coverage and can be found in various regions that were once covered by ice. Additionally, other geological features such as drumlins and glacial till also provide evidence of the ice sheets' advance and retreat.
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.
Some famous moraines in the US include the terminal moraine of the Wisconsin glaciation in Long Island, New York, and the moraines left behind by the glaciers in Glacier National Park in Montana and Denali National Park in Alaska.
continental creates smooth peaks just remember the smoothe curved c edge is smooth>C Alpine creates sharp rugged peaks like the sharp point on the A
The Canadian shield
I think it
Glaciation had a significant impact on the Earth's landscape by shaping valleys, creating moraines, and depositing sediments as the glaciers advanced and retreated. It also played a role in influencing global climate patterns and sea levels through changes in albedo and the release of freshwater into the oceans.
Geographers conclude that moraines are indicators of past glacial activity. These ridgelike piles of rock and debris are formed from the accumulation of materials that glaciers have eroded and transported as they advance and retreat. The presence and characteristics of moraines can reveal information about the movement and size of glaciers, as well as the environmental conditions during the periods of glaciation.
The Great lakes went through glaciation many thousands of years ago.
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.
Glaciation can benefit ecosystems by creating diverse habitats for plants and animals, helping with soil fertility through sediment deposits, and shaping landscapes with unique geological features like moraines and valleys. Glaciers also play a role in regulating global climate by reflecting sunlight, contributing to temperature stability.
Depends on what is meant by the word 'features'. Alpine glaciation tends to create certain recognizable features like cirques and U-shaped valleys, and the sediments plucked by the glaciation can be traced back to their source by careful examination.
Kames. Many are found in areas of kettles and moraines.