I know three: morains (a hill of dirt and rocks where the glacier stopped moving and then melted), carved valleys that are U-shaped vs. those valleys cut by a stream or river, rocks that are very smooth because of the ice and rocks they slid over.
The feature that is the result of a glacier carving out rock as it moves is a roche moutonnees. It is a rock formation created by the passage of glacier ice. Or a terminal moraine
A feature that is not the result of a glacier carving out rock is a delta. Deltas are formed by the deposition of sediment carried by a river as it flows into a larger body of water, such as an ocean or lake, rather than through the erosive action of a glacier. In contrast, features like U-shaped valleys and glacial striations are directly caused by glacial movement and erosion.
A moraine is formed by a glacier. A moraine may be terminal, medial, or lateral.
an esker is formed by a Glacier
The name of a glacier that has frozen to bedrock is rock glacier. A rock glacier is formed by angular blocks of frozen rock that form in the valley of glaciers.
Hanging valleys are formed when smaller glaciers flowing from tributary valleys join a larger glacier in a main valley. As the larger glacier is more powerful, it erodes the main valley deeper than the tributary valleys. This results in the tributary valleys being left at higher elevations once the glaciers retreat, creating the characteristic "hanging" appearance.
A tributary glacier is like a glacier to the side of the main glacier, oftem separated by a land form.
In cross-section: A 'U' shaped valley is formed from glacial erosion. A 'V' shaped valley is formed by river erosion.
a moraine
Stratified drift
A nose is not a feature carved out by a glacier. If you want to ask a multiple choice question on this site, you have to include the choices in the question.
The feature that is the result of a glacier carving out rock as it moves is a roche moutonnees. It is a rock formation created by the passage of glacier ice. Or a terminal moraine
A cirque is a surface feature formed by glaciers that is shaped like an armchair. It is a large bowl-like depression with steep walls carved out by the glacier's erosion.
A medial moraine is formed by deposition. It is a ridge of glacial debris that runs down the center of a glacier where two tributary glaciers merge. The debris is deposited as these glaciers flow and carry rock material with them, which accumulates in the center of the combined glacier.
Terminal moraines are not formed due to erosion but rather deposition. They are ridges of glacial till that mark the farthest advance of a glacier and are deposited as the glacier retreats. Erosion by the glacier does contribute to the material found in terminal moraines, but the feature itself is primarily a result of deposition.
Glacial Trough (U-shaped valleys) - Flat-bottomed valley with steep sides produced by the erosion of the floor and sides of the valley by an alpine glacier as its sediment abrades while the glacier flows downhill. On the topographic maps they are recognized by closely spaced contours along the valley sides and widely spaced contours on the valley floor.Hanging Glacial Troughs - Formed when the down-cutting erosion of the main valley glacier exceeds that by the tributary glacier. The tributary glacier flows onto the main glacier and thus has an erosional base level of the elevation of the main valley glacier. After melting, the lower portion of the tributary glacial trough is then left hanging above the main floor of the glaciated valley. On maps they are recognized by more widely spaced contours across a stream in the upper portion than in the lower portion (where the modern stream cascades into the main valley below).
The total length of glacier feature labeled "a" is 1 mile.