Cirques and U-shaped valleys are formed by glacial erosion. Cirques are formed by the erosive action of a glacier in a bowl-shaped depression at the head of a valley. U-shaped valleys are carved out by glaciers as they flow down a mountain, eroding the surrounding rock and creating a distinctive U-shape.
Cirques intersect at their highest point, where the walls of adjacent cirques meet to form a sharp ridge or crest called an arête. This intersection often occurs at a mountain peak or ridge line.
Glacial erosion can form various landforms like cirques, arêtes, and valleys. As glaciers move, they pick up rocks and debris, which can carve out shallow grooves known as striations on the underlying rock. When the glacier retreats, it leaves behind moraines made up of this debris.
Glacial ice erosion will form: * Corries (cirques) * Aretes * Pyramidal Peaks * U-shaped troughs * Hanging Valleys * Truncated Spurs * Rouche Moutonees * Striations * Rock Steps Sediment deposition (resulting from glacial processes) will form: * Ice-transported boulders * Erratics * Lateral moraines * Medial moraines * Terminal moraines * Recessional moraines * Push moraines * Varves * Eskers * Delta kames * Kame terraces * Braided streams * Flat bottoms to U-shaped valleys
Valleys can be formed by a combination of erosion and weathering. Erosion, which is the process of wearing away rock and soil, contributes to the shaping of valleys by moving sediment and carving out the land. Weathering breaks down rocks and contributes to the gradual formation of valleys over time.
Alpine glaciers form in mountainous regions and are confined within valleys or cirques, while continental glaciers are large ice sheets that cover vast land areas. Alpine glaciers are typically smaller and more fragmented compared to the continuous ice sheets of continental glaciers.
this is a peproduction
Cirques and U-shaped valleys are primarily formed by glacial erosion. Glaciers moving downhill erode the surrounding rock through processes like plucking and abrasion, creating the characteristic amphitheater shape of cirques and the broad, steep-sided valley of U-shaped valleys. These landforms are typically found in areas that have experienced past glaciation.
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.
The plural form of "valley" is "valleys."
Glaciers can form various landscape features, including U-shaped valleys, cirques, aretes, and moraines. These features are created as glaciers erode and deposit material as they flow over the land.
Cirques intersect at their highest point, where the walls of adjacent cirques meet to form a sharp ridge or crest called an arête. This intersection often occurs at a mountain peak or ridge line.
The plural form is valleys. The plural possessive is valleys'.
terminal moraines--------------------------------------------------------------------------------------------------------They can be:Cirques, bowl-shaped depressions where glacial ice cuts back into the mountain walls.Horns, sharp, pyramid-like peaks that form when three or more alpine glaciers carve a mountain.Arête, a jagged ridges that form between two or more cirques that cut into the same mountain.Also U-shaped valleys and Hanging Valleys.
Moraine
The plural form is valleys. The plural possessive is valleys'.
rift valleys form by tension stress
Answer: Cirques