erosion
deposition
weathering
and a lot more...
The gradient typically decreases as you move from the headwaters to the mouth of a stream. This is because the elevation drops and the slope becomes gentler downstream.
An increase in precipitation, snowmelt, or glacial melt can cause a stream's discharge to increase. Additionally, if there is a sudden influx of water from a tributary or a dam release upstream, it can also lead to an increase in stream discharge.
Stream gradient, or the slope of the stream channel, affects stream velocity by influencing the speed at which water flows downstream. A steeper stream gradient typically results in a faster water flow velocity, as the force of gravity pulls water downhill more strongly. Conversely, a gentler stream gradient leads to slower water flow velocity.
rate of stream discharge is directly proportional to the erosion i.e the higher the velocity of the stream then it will erode the rock rapidly while the deposition process will be slow when the velocity will be high.
If the water table rises, the stream may become more full and flow faster due to increased groundwater discharge into the stream. This could potentially lead to flooding and erosion along the stream banks.
Decrease. The source of the river is usually in a mountainous area with a steep gradient.
pressure, temperature, possibly somethign else
A stream's velocity typically increases downstream due to the accumulation of water volume and slope gradient. This leads to higher flow rates and faster-moving water.
A decrease in water velocity usually causes more sediments to be deposited at a location in a stream. This can happen when the stream widens, the channel gradient decreases, or obstacles such as rocks or vegetation slow down the flow of water.
Yea
The gradient typically decreases as you move from the headwaters to the mouth of a stream. This is because the elevation drops and the slope becomes gentler downstream.
Stream discharge would increase if additional water enters it, such as from a rain storm or from melting snow.
Decrease in stream velocity
Decrease in stream velocity
Decrease in stream velocity
A decrease in stream velocity due to factors such as a decrease in slope or widening of the stream channel can cause sediment to be deposited. When the stream's capacity to transport sediment is exceeded, it drops the sediment it was carrying. Additionally, changes in the stream's flow rate or turbulence levels can also result in sediment deposition.
The width of the stream will increase as the order increases