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Decrease in stream velocity
A stream deposition occurs when, in the lower reaches, the flow of water (speed of flow) is reduced. Which is when the heavier sediment falls out and settles on the river bed.
Deposition, whereby the sediment load being transported is dropped.
what weathering does is that weathering moves your soil or sediments and then when it hits a stream erosion happens and moves it down along the stream and then comes deposition and the sediment lands at a random spot.
It is because if a stream gets bigger, it is allowed to carry more sediment. More sediment means more erosion.
J. M Knott has written: 'Sediment discharge data for selected sites in the Susitna River Basin, Alaska, 1981-82' -- subject(s): Sedimentation and deposition 'Sediment transport characteristics of selected streams in the Susitna River Basin, Alaska' -- subject(s): Stream measurements, Sedimentation and deposition, Bed load, Sediment transport, Measurement 'Sediment transport characteristics of selected streams in the Susitna River Basin, Alaska, October 1983 to September 1984' -- subject(s): Stream measurements, Sediment transport, Sedimentation and deposition
Typically, when the earth's surface is exposed to the impacts of rainfall, there is an increase in the volume and velocity of runoff. This sets off a chain reaction that results in the transport and deposition of sediment, reduced stream capacity, and ultimately increased stream scour and flooding.
It is called deposition. It occurs as friction or gravity overcomes the force of the moving water.
A moraine is a place of deposition for a glacier. It contains unsorted till, or sediment. A meander is a type of stream. It is a long curvey stream that moves slowley. Meaders are found in plain type areas
Sediment that is carried by a stream along the bottom of its channel.
Charles L Whittington has written: 'Analytical results of stream-sediment samples from the Medford 1p0s' -- subject(s): Sedimentation and deposition, Geochemistry
Stratification as this is a term that describes the layering of rocks and so is not a term that is related to sediment transport (i.e. erosion) but is instead the result of deposition, compaction and cementation.