Answer: Cirques
It is formed when two glaciers erode parallel from each other or when two glaciers erode towards each other
These are glaciers.
Glaciers erode Earth's surface through abrasion, where the ice and sediments grind against the rock, wearing it down. They also erode through plucking, where the glacier freezes onto rock and plucks or pulls it away as the glacier moves.
Glaciers erode by abrasion when they drag rocks and sediments along their base and sides, creating a sandpaper effect. This process occurs as the glacier moves, grinding, scratching, and smoothing the underlying bedrock and carving out deep valleys. The debris carried by the glacier further enhances the abrasion process as it scrapes against the surface.
Glaciers create various landforms such as U-shaped valleys, moraines, drumlins, and fjords through processes like erosion, deposition, and melting. For example, as glaciers move, they erode the land beneath them, forming U-shaped valleys. When glaciers retreat, they leave behind piles of debris called moraines. Drumlins are elongated hills formed by glaciers depositing sediments, and fjords are deep, narrow inlets created by glaciers moving through valleys and subsequently melting.
Yes
It is formed when two glaciers erode parallel from each other or when two glaciers erode towards each other
Yes ... usually from heat.
These are glaciers.
Yes, glaciers erode the base of mountains into basins called cirques through the process of glacial erosion. As a glacier moves down a mountainside, it plucks and abrasively scrapes the rock beneath, creating a bowl-shaped depression called a cirque. Over time, these cirques can deepen and widen, forming distinctive features in mountainous regions.
by your mom. ok?
abrasion and plucking.
Plucking and Abrasion.
The glacier can carry rocks. The moving of the glacier.
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.
Sharp pyramid-shaped peaks formed by alpine glaciers are called horn glaciers. Horn glaciers are created when three or more cirque glaciers erode a mountain from different sides, leaving behind a sharp-edged peak. Famous examples include the Matterhorn in the Alps.
glacial deposition and glacial erosion