Deposition creates landforms such as alluvial fans and deltas.It can also add soil to a river.
Hope this helps.
stream turns into green water
High or low pressure lies along the subtropical jet stream, depending on the time of year. The pressure gradient follows the path of the jet stream.
When other rivers or lakes join to the main river . It is called the tributary .
yes...along with a chart or table too
Matter
often salt or potassium in other cases
stream turns into green water
stream turns into green water
deposition, ground water, delta
The course along which waters move
cilt and dirt and also rocks can settle along a stream. over time this can effect the dimmessions of the stream. deposition would be the depositing of rocks dirt and cilt or the settling of these materials. this could make the walls closer in or the depth to become smaller ultimately makeing the stream smaller, allowing less water to flow.
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.
deposition, ground water, delta
The elevation down to which a river has the ability to erode its bed everywhere along its course.
As water flows, it picks up particles of the ground and carries it along the stream of water. That is erosion. As water deposits into another body of water, for example the Mississippi river into the Gulf of Mexico, those particles of ground are deposited in that area. That is deposition.
The elevation down to which a river has the ability to erode its bed everywhere along its course.
The deposition of sediment along the mouth of the river was great.
flat land area adjacent to a stream, composed of unconsolidated sedimentary deposits (alluvium) and subject to periodic inundation by the stream. Floodplains are produced by lateral movement of a stream and by overbank deposition; therefore they are absent where downcutting is dominant. Any erosional widening of one bank is approximately equalled by deposition on the opposite side of the channel in the form of bar development along the inside of meander bends. Thus, the simplest floodplain is made up of a strip of sinuous scrolls immediately adjacent to the stream.