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It flows slower because when a river goes down it flows faster because gravity is helping it and when its on a flat area it doesn't move as fast because gravity isn't help pull the water down therefore making it slower.

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When a river floods would its water flow faster or slower than its normal speed?

When a river floods it water will flow faster then the normal speed.


What is the flat plain land through which a river flow called?

old river


Why is more silt in water found on flatland?

Silt settles out of water more readily in flat areas because there is less turbulence to keep it suspended. In flat land, water flow is usually slower, allowing silt particles to settle to the bottom. Silt is also more likely to accumulate in low-lying areas where water pools and has less opportunity to flow.


What is the advantage of having slower blood flow in some areas of the body such as the capillaries of our fingers?

The advantage of having slower blood flow in some areas of the body is simple. If blood isn't going to theses areas they are going to more important areas of the body like the brain.


Does a river flow faster in mountains or on a plain?

Well....... It depends. If the river is really big and wide, and there are hardly any plants growing in it, and there are no rocks and the river is on a plain, then it will probably flow really fast. If the river is atiny little stream in the mountains, then it will probably flow slower. It all depends on the river


What is the difference between a young and mature a river?

A young river typically has a fast flow rate, steep gradient, and v-shaped valley, while a mature river has a slower flow rate, gentle gradient, and wide, flat valley. Young rivers are more erosive, carrying a lot of sediment, while mature rivers have a more stable channel and deposit sediment.


Clay and silt are found in what part of the river?

If the river is moving slower than ~0.01 cm/sec, then clay may be found in the river bed. If it is slower than ~0.3 cm/sec, then silt may be found. Any faster and the clay and silt would be deposited at the mouth of the river where the velocity decreases greatly.


What kind of rivers travel slow?

Slow-moving rivers typically have gentle gradients, meandering courses, and wider channels. They often flow through flat or low-lying areas, allowing sediment to accumulate and creating features like oxbow lakes and wetlands. Additionally, rivers that receive significant inflow from lakes or are influenced by human activities, such as damming, can also exhibit slower flow rates. Examples include the Mississippi River and the Amazon River in certain sections.


Would you expect to see a river in a mountain or plain region?

You are more likely to see a river in a plain region. Rivers typically originate from higher elevations, such as mountains, and flow downhill into lower-lying areas like plains. While rivers can exist in both mountain and plain regions, they are more prevalent and prominent in plain regions due to the flatter terrain that allows for slower and more meandering flow.


What are the areas of sediment deposit where a rivers mouth reaches flat land at the bottom of a mountain?

The areas of sediment deposit where a river's mouth reaches flat land at the bottom of a mountain are known as alluvial fans. Alluvial fans are cone-shaped landforms that are created by the deposition of sediment carried by rivers as they flow from steep mountain terrain to flatter regions. The sediment is deposited at the base of the mountain due to a decrease in flow velocity as the river enters the flatter area.


Which south american river flow through lowland areas?

The Paraguay River flows through lowland areas in South America, specifically in countries like Brazil, Paraguay, and Argentina. Its course passes through the Gran Chaco region, which is known for its flat and low-lying plains.


What stage of a river do meanders form?

Meanders typically form in the middle stage of a river, where the flow is slower and the riverbed is relatively flat. In this stage, the water erodes the outer banks and deposits sediment on the inner banks, creating the characteristic winding curves. Over time, these meanders can become more pronounced as the river continues to erode and deposit sediment.