A deposit of rock particles that are scratched and unsorted has most likely been transported and deposited by glacial ice.
A glacial moraine typically contains unsorted and unlayered sediment that was transported and deposited by a glacier. The sediment can range in size from tiny clay particles to large boulders, with no specific sorting according to size. It is a mixture of debris from the glacier's abrasion and plucking processes.
Moraines are composed of a mixture of rocks, gravel, sand, and clay that have been transported and deposited by glaciers. They are typically unsorted and can vary in size from tiny particles to large boulders.
The unsorted rock material deposited directly by a melting glacier is called till. Wind erosion that removes dry soil particles is known as deflation. Together, these processes can create a landscape called a desert pavement where larger rocks are left behind due to deflation.
Yes, a moraine is formed by glacial deposition. It is a landform made up of unsorted rock material (till) that has been transported and deposited by a glacier as it moves and melts.
Glacial ice is the most probable agent of erosion that deposited unsorted sediments in deposit B. Glaciers can transport a wide range of sediment sizes and mix them together as they move, resulting in unsorted sediments.
unsorted and not layered :)
A glacial moraine typically contains unsorted and unlayered sediment that was transported and deposited by a glacier. The sediment can range in size from tiny clay particles to large boulders, with no specific sorting according to size. It is a mixture of debris from the glacier's abrasion and plucking processes.
Moraines are composed of a mixture of rocks, gravel, sand, and clay that have been transported and deposited by glaciers. They are typically unsorted and can vary in size from tiny particles to large boulders.
The unsorted rock material deposited directly by a melting glacier is called till. Wind erosion that removes dry soil particles is known as deflation. Together, these processes can create a landscape called a desert pavement where larger rocks are left behind due to deflation.
Yes, a moraine is formed by glacial deposition. It is a landform made up of unsorted rock material (till) that has been transported and deposited by a glacier as it moves and melts.
Glacial ice is the most probable agent of erosion that deposited unsorted sediments in deposit B. Glaciers can transport a wide range of sediment sizes and mix them together as they move, resulting in unsorted sediments.
Glaciers are the agent of erosion that deposit irregular mounds of unsorted sediment with parallel scratches on rounded particles. This type of deposit is called a moraine, which is formed as the glacier moves and carries a mixture of different-sized sediments that get deposited when the glacier melts.
Till is a mixture of sediment and rock that is deposited directly by a glacier, while outwash is the material carried away from a glacier by meltwater and deposited in a different location. Till tends to be unsorted and can have a range of sizes of particles, while outwash is typically well-sorted and composed of smaller particles.
The accumulation of unsorted rocky debris that is formed by a melting glacier is called a moraine. There are many large moraines throughout the northern parts of North America, Europe, and Asia.
The unsorted rocky debris formed by a melting glacier is known as glacial till. This mixture of rock fragments of various sizes and shapes is deposited by the glacier as it retreats, with no specific order or arrangement. Glacial till can form different landforms, such as moraines or drumlins, depending on how it is deposited.
Till is unsorted and unstratified glacial sediment, consisting of a mix of different-sized particles. It can contain a wide range of rock types and sizes, from clay to boulders. It is often deposited directly by the moving glacier as it retreats.
Unsorted rocky debris that is formed during the melting of a glacier is known as a till. When there are many tills that are present the sediment that is deposited forms a till plain.