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.
Moraines, aretes, cols, horns, and cirques. As a glacier flows downward (even when retreating it's still flowing downhill) it is cycling dock debris, called glacial till, throughout itself. The till gets deposited along the sides of the glaciers, forming lateral moraines. When the glacier is stable in one location (when the rate of melting is equal to the rate of flowing), a terminal moraine forms at the nose of the glacier.
Cirques are the large bowls left on the mountain where the glacier came from. Horns are where three or four cirques all come together (look at a picture of the Matterhorn). Aretes are knife like rides either between two cirques or glacial valleys. Cols are low spots within cirques or aretes, usually named as passes.
Glacial valleys are U-shaped. A lake in a cirque is a tarn.
valleys, mountains, canons, lakes, rivers, and hills.
a glacier next to a glacier A glacier that flows into a larger glacier.
I used this website, http://www.answers.com/topic/tributary-glacier
Some features that are formed by glaciers are crevasses, which are large cracks or fissure in a glacier, ice shelves, and icebergs... (<--- The Titanic, LOL xD)
Pyramidal peaks, arêtes, cirques, U-shaped valleys, assorted moraines, drumlins and eskers are among the many features formed by glaciers.
A hanging valley.
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 moraine is formed by a glacier. A moraine may be terminal, medial, or lateral.
an esker is formed by a Glacier
Cirques
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.
A tributary glacier is like a glacier to the side of the main glacier, oftem separated by a land form.
a moraine
In cross-section: A 'U' shaped valley is formed from glacial erosion. A 'V' shaped valley is formed by river erosion.
it is formed by a glacier
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).
An alpine glacier is a glacier that FORMED on a mountain. It doesn't have to BE on a mountain, just formed on one.
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
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
By a glacier
ice
yes from the cintinental period a glacier swept acrost and made a hole and the glacier melted and formed the salt lakes
A tarn (or corrie loch) is a mountain lake or pool, formed in a cirque excavated by a glacier.