Current ripple marks
A boulder is the largest piece of sediment.
What is the name for wind blown sediment
Any and all rock can be changed into sediment by weathering and erosion.
When organisms died in a river or stream of some sort, they are covered in a layer of sediment, as time gos by the sediment hardens and is covered by another layer of sediment and so on.
Sediment is the stuff that settles at the bottom of a liquid (such as the bottom of a pond). It can include sand and pebbles but also dead plants and animals. If conditions are right, the sediment can dry out and turn into a sedimentary rock (a rock made from sediment). Sedimentary rocks can contain fossils of plants or animals that fell into the "muck" at the bottom of a body of water. Cool, huh?
The transport of sediment depends on its grain size and the original location where it was produced. Terrigenous sediment can be transported to the deep sea via rivers or by wind. Material transported by rivers most commonly ends up deposited on thecontinental margin, the shallow portions of the ocean that are within several hundred kilometers of land. When continental margin deposits accumulate fast and get overly steep, or when an earthquake or storm causes the sediment to be resuspended, turbidity currents provide additional transport out to the deep sea. The resuspension of the sediment into the bottom water causes it to be more dense than the overlying water, and thus these turbidity currents flow downslope to the more distant ocean basin -humberto <3
The transport of sediment depends on its grain size and the original location where it was produced. Terrigenous sediment can be transported to the deep sea via rivers or by wind. Material transported by rivers most commonly ends up deposited on thecontinental margin, the shallow portions of the ocean that are within several hundred kilometers of land. When continental margin deposits accumulate fast and get overly steep, or when an earthquake or storm causes the sediment to be resuspended, turbidity currents provide additional transport out to the deep sea. The resuspension of the sediment into the bottom water causes it to be more dense than the overlying water, and thus these turbidity currents flow downslope to the more distant ocean basin -humberto <3
The transport of sediment depends on its grain size and the original location where it was produced. Terrigenous sediment can be transported to the deep sea via rivers or by wind. Material transported by rivers most commonly ends up deposited on thecontinental margin, the shallow portions of the ocean that are within several hundred kilometers of land. When continental margin deposits accumulate fast and get overly steep, or when an earthquake or storm causes the sediment to be resuspended, turbidity currents provide additional transport out to the deep sea. The resuspension of the sediment into the bottom water causes it to be more dense than the overlying water, and thus these turbidity currents flow downslope to the more distant ocean basin -humberto <3
Deposition, whereby the sediment load being transported is dropped.
Longshore Currents transport most sediment along the shore of beaches, according to my science book. .
Aeolian deposits.
Is the sediment carried by the waves and the currents
i need help
Sediment that is carried by a stream along the bottom of its channel.
igneous rock
a bedload
It is called deposition.