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.
When sediments deposit in lakes or oceans, they typically settle in layers on the bottom of the body of water. Over time, these layers can build up and form sedimentary rock.
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.
A thick deposit of windblown fine-grained sediments is called loess. This sediment is typically uniform, composed of silt-sized particles, and can be found covering large areas of land.
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.
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.
When sediments deposit in lakes or oceans, they typically settle in layers on the bottom of the body of water. Over time, these layers can build up and form sedimentary rock.
beach
accumulated sediments on the bottom of the river
Drift and/or till.
till
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.
A thick deposit of windblown fine-grained sediments is called loess. This sediment is typically uniform, composed of silt-sized particles, and can be found covering large areas of land.
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.
no
turbidity currents deposit sediments on the ocean floor
A landform created when a river reaches a large body of water and deposits sediments is called a delta. Deltas are typically triangular or fan-shaped and form where the river's velocity decreases, causing it to deposit the sediments it has been carrying.
Some are and some aren't. Infauna just refers to animals that live in the sediments. If they extend feeding appendages out into the water to capture prey (like mud anemones for example) , then they're not deposit feeders. If they remove organic matter from the sediments, they're deposit feeders. Most benthic infauna are deposit feeders.