Well really the valleys BETWEEN hills form by glacial and/or other erosion. The hills are what's left behind.
Arêtes can form in two ways. They can form when two glaciers erode parallel U-shaped valleys, or they can form when two glacial cirques erode headwards toward one another, although frequently this results in a saddle-shaped pass, called a col.
fortniye
Glacial valleys (also known as glacial troughs) tend to be u-shaped, as opposed to river valleys which are v-shaped.
When a glacier melts, it deposits sediment in various landforms known as glacial landforms. These include moraines, which are accumulations of debris at the glacier's edge, drumlins, which are elongated hills shaped by the glacier's movement, and outwash plains, formed by meltwater transporting and depositing sediments beyond the glacier's terminus. These features reflect the dynamic processes of glacial erosion and deposition, shaping the landscape as the ice retreats.
Glacial erosion is the process by which a glacial flows over the land, picking up rocks. Glacial deposition is the process by which a glacier gathers a huge amount of rock and soil as it Erodes the land in the path
Two types of glacial deposits are moraines, which are formations of mixed sediment pushed by and deposited from a glacier, and drumlins, which are elongated hills made of glacial till that form parallel to the direction of ice flow.
"Moraine" hills,...caused by glacial deposits while receding.
The word erosion is a noun. The plural form is erosions.
drumlins
drumlins
Eskers
No
Moraines, drumlins, eskers, and outwash plains are glacial features that result from deposition. Moraines are ridges of till deposited along the edges of a glacier, drumlins are elongated hills of glacial till, eskers are long, winding ridges of sand and gravel, and outwash plains are flat areas of sand and gravel deposited by meltwater streams flowing away from the glacier.
Approximately 69%
there are three reasons first the wind the rain the magma and the erosions
Glacial Erosion formed Yosemite Valley and the Sierra Nevada
During the last Ice Age, glaciers covered the eastern part of South Dakota, particularly the region known as the Glacial Lake Dakota area. This glaciated region features rolling hills and plains shaped by glacial activity. The western part of South Dakota, including the Black Hills, remained largely unaffected by glacial coverage.