Wind or water carrying sediment deposits its load in slow moving or standing water. Sediment typically comes from beaches, erosion, and typical weathering.
sedimentary rocks :)
Alluvial deposits refer to sediments deposited by streams. These deposits are typically composed of sand, gravel, and silt that are carried and deposited by flowing water.
When water loses its ability to hold sediment due to a decrease in velocity or capacity, it deposits the sediments it was carrying. This process is called sedimentation, and it can result in the formation of sedimentary layers over time.
Alluvial deposits, which are created by the movement of water and include sediments like sand, clay, and gravel. Glacial deposits, formed by the movement and melting of glaciers, leaving behind materials such as moraines, till, and outwash. Delta deposits, which are sediment accumulations at the mouths of rivers where water flow slows and sediment is dropped, forming features like distributaries and levees.
A river that deposits only small particles is most likely to be slow. This is because slower water flow lacks the energy to carry larger sediments, allowing only smaller particles, like silt and clay, to be transported and deposited. In contrast, fast-flowing rivers can carry larger sediments due to their higher energy.
Delta.
Water erosion utilizes water to carry sediments away.
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.
The erosion agent that typically deposits hills of unsorted sediments is glacial activity. As glaciers move, they carry a mixture of sediments, including clay, silt, sand, and larger rocks, without sorting them by size. When glaciers melt, they leave behind these unsorted deposits, known as till, which can form features such as drumlins or moraines. This process contrasts with other erosion agents like water or wind, which tend to sort sediments by size.
Air ,ice ,gravity ,and water
Sediments can be picked up by water, wind, or ice. Water can transport sediments in rivers, streams, and oceans, while wind can carry sediments in the form of dust or sand. Ice, through processes like glaciers, can also transport sediments across landscapes.
Sedimentary rock is formed from sediments deposited in bodies of water. Examples of sedimentary rocks that can form in this way include limestone, shale, and sandstone. These rocks are typically composed of particles that have been weathered, transported, and compacted over time.