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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.

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A deposit of rock particles that are scratched and unsorted has most likely been transported and deposited by what?

The deposit is most likely transported and deposited by a glacier. Glaciers are massive sheets of ice that can carry rock particles long distances and leave behind unsorted and scratched deposits as they melt and retreat. This process is known as glacial deposition.


Which erosional agent typically deposit hills of inspected sediments?

Wind is a common erosional agent that can deposit hills of unsorted sediments called dunes. These dunes are often found in arid or coastal regions where wind can transport and deposit sand or silt to form distinct mound-like features.


What are the materials deposited by water wind and melting glaciers?

Water can deposit sediment such as sand, silt, and clay. Wind can deposit smaller particles like sand and dust. Melting glaciers can deposit a mixture of rocks, sediments, and debris known as moraines.


What is the difference between a till and a moraine?

A till is an unsorted mixture of sediment deposited by a glacier, while a moraine is a landform made up of till deposited at the edge or beneath a glacier. Tills are deposited directly by the moving glacier, while moraines are created from the accumulation of till as the glacier advances, retreats, or melts.


Is a moraine sorted or unsorted?

A moraine is unsorted. Plucking and abrasion by glaciers do not discriminate in size of material debris. It might grind rock matter into what is called "rock flour" and this may be visible at the snout of a glacier, but this and other debris of any size will be be deposited as unsorted till in the form of an end moraine (terminal moraine). A moraine between 2 glaciers is a medial moraine, a moraine along side the glacier is a lateral moraine. Sometimes till can contain glacial erratics... that is, material that came from very far away and does not fit with other materials in the till deposit. Glaciers act as a conveyor belt depending on budget, and material moves with the plasticity of the ice. I hope this helps a little bit.

Related Questions

A deposit of rock particles that are scratched and unsorted has most likely been transported and deposited by what?

The deposit is most likely transported and deposited by a glacier. Glaciers are massive sheets of ice that can carry rock particles long distances and leave behind unsorted and scratched deposits as they melt and retreat. This process is known as glacial deposition.


Which agent of erosion deposits irregular mounds of unsorted sediment with parallel scratches on rounded particles?

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.


Are there any rivers that deposit and eroded sediments?

Most rivers have eroded and Deposited sediment.


Which erosional agent typically deposit hills of inspected sediments?

Wind is a common erosional agent that can deposit hills of unsorted sediments called dunes. These dunes are often found in arid or coastal regions where wind can transport and deposit sand or silt to form distinct mound-like features.


What are the materials deposited by water wind and melting glaciers?

Water can deposit sediment such as sand, silt, and clay. Wind can deposit smaller particles like sand and dust. Melting glaciers can deposit a mixture of rocks, sediments, and debris known as moraines.


What are unsorted deposits?

Unsorted deposits refer to sedimentary deposits that have not been sorted or arranged by size or weight. This means that the particles or materials within the deposit have not undergone any sorting process based on their characteristics, such as size, shape, or density. Examples of unsorted deposits include moraines left by glaciers or alluvial fan deposits.


What is a glacial till?

Glacial till is a type of sediment deposited by glaciers through the process of erosion and transportation. It is a mixture of different sized particles, ranging from clay to boulders, that is left behind as the glacier melts. Glacial till is an unsorted and unstratified deposit.


Why do some glacial deposition have sorted sediments while others do not?

Glacial sediments that are sorted are due to flowing water in the glacier. Unsorted sediments are those that have thawed out of the ice randomly.


What is the difference between a till and a moraine?

A till is an unsorted mixture of sediment deposited by a glacier, while a moraine is a landform made up of till deposited at the edge or beneath a glacier. Tills are deposited directly by the moving glacier, while moraines are created from the accumulation of till as the glacier advances, retreats, or melts.


Is a moraine sorted or unsorted?

A moraine is unsorted. Plucking and abrasion by glaciers do not discriminate in size of material debris. It might grind rock matter into what is called "rock flour" and this may be visible at the snout of a glacier, but this and other debris of any size will be be deposited as unsorted till in the form of an end moraine (terminal moraine). A moraine between 2 glaciers is a medial moraine, a moraine along side the glacier is a lateral moraine. Sometimes till can contain glacial erratics... that is, material that came from very far away and does not fit with other materials in the till deposit. Glaciers act as a conveyor belt depending on budget, and material moves with the plasticity of the ice. I hope this helps a little bit.


What is the deposit of sediments parallel to the shore?

beach


What is a thick deposit of windblown fine grained sediments?

A thick deposit of windblown fine-grained sediments is called loess. Loess is typically composed of silt-sized particles that have been carried by the wind and deposited over time, creating distinct layers of sediment. Its properties make it a fertile soil that is often used for agriculture.