It could be two things, either plucking, a form of glacial erosion where weak rock is moved or erratics, which is a form of glacial deposition in which rocks, even car size, are transported by glacial ice into a region with different bedrock.
A large thick body of slow-moving ice is called a glacier. Glaciers form over time as snow accumulates and compacts into ice, flowing downslope under the force of gravity. Glaciers can reshape the landscape as they erode rocks and carry sediments.
Large rocks can be transported by natural processes such as glaciers, rivers, and ocean currents. These processes are capable of moving rocks of various sizes over long distances by erosion, deposition, and ice movement.
Glaciers are able to carry large particles with ease due to their immense size and weight, which provides the necessary force to move and transport these particles. The ice in glaciers acts as a lubricant, reducing friction between the glacier and the ground, allowing it to slide and carry debris more easily. Additionally, the slow but continuous movement of glaciers over time helps to accumulate and transport large particles along their path.
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.
Glaciers contribute to physical weathering through a process called abrasion, where the movement of ice and rock fragments scours and erodes the underlying bedrock. As glaciers move, they pick up and carry large boulders and rocks that act as tools to grind and shape the landscape beneath them. Over time, this process can create valleys, fjords, and other glacier-carved landforms.
The glacier can carry rocks. The moving of the glacier.
A large thick body of slow-moving ice is called a glacier. Glaciers form over time as snow accumulates and compacts into ice, flowing downslope under the force of gravity. Glaciers can reshape the landscape as they erode rocks and carry sediments.
Large rocks can be transported by natural processes such as glaciers, rivers, and ocean currents. These processes are capable of moving rocks of various sizes over long distances by erosion, deposition, and ice movement.
Glaciers are able to carry large particles with ease due to their immense size and weight, which provides the necessary force to move and transport these particles. The ice in glaciers acts as a lubricant, reducing friction between the glacier and the ground, allowing it to slide and carry debris more easily. Additionally, the slow but continuous movement of glaciers over time helps to accumulate and transport large particles along their path.
When wind, water, and glaciers carry away rocks, the process is known as erosion. Wind can dislodge and transport small particles, while flowing water, such as rivers and streams, can carry larger rocks and sediments over great distances. Glaciers, through their immense weight and movement, grind and transport rocks and debris as they advance and retreat. These natural forces shape landscapes and contribute to the formation of various geological features.
These are glaciers. Glaciers are large bodies of ice that flow slowly over land, eroding the landscape and carrying rocks and soil with them as they move.
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.
Glaciers contribute to physical weathering through a process called abrasion, where the movement of ice and rock fragments scours and erodes the underlying bedrock. As glaciers move, they pick up and carry large boulders and rocks that act as tools to grind and shape the landscape beneath them. Over time, this process can create valleys, fjords, and other glacier-carved landforms.
A glacier. Glaciers are large masses of ice that slowly move downhill, eroding the land and carrying debris like rocks with them.
The scratch marks on rocks left by moving glaciers are called glacial striations. These marks are typically parallel and indicate the direction in which the glacier was moving.
Glaciers are not made of rock; they are made of ice. Glaciers can contain rocks, but not of any particular type. Rather, they carry whatever type of rock they are going over or have gone over.
Glaciers can transport and deposit large amounts of soil, rocks, and gravel as they move. This process, called glaciation, can erode bedrock and reshape landscapes. Glacial deposits can also create distinctive landforms like moraines, drumlins, and eskers.