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Stream/River Erosion & Deposition
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A river is simply a LARGE stream!!
What is a Stream/River? A stream is a moving body of water that eventually connects to an ocean A river is simply a LARGE stream!!
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Which river has a greater velocity?
Stream / River Characteristics Velocity – how fast or slow the river is moving. This determines the rivers ability to erode sediments Which river has a greater velocity?
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Stream / River Characteristics
2. Gradient – the slope or steepness of the river The steeper the gradient, the more energy
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Stream / River Characteristics
3. Discharge – the amount of water moving by a certain point of the river in a set time The Amazon River in South America has greatest discharge 212,400 m3/s Mississippi River in USA has 7th greatest discharge at 17,300 m3/s
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Stream / River Characteristics
4. Stream Channel – the course that the water flows in a river
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Following a River from Source to Mouth
A river begins at the source/headwaters This is usually where you find the steepest gradient You may also find V-shaped valleys here
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Following a River from Source to Mouth
Alluvial Fan: A fan-shaped deposit of sediment that forms when a stream drops downward from a higher elevation and encounters the valley floor. The stream slows down, depositing fine silt, sand, or other sediments it is carrying.
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Waterfall Formation The stream bed has soft and hard rock.
The softer rock erodes MORE QUICKLY as the river flows over it. Eventually there is a big enough difference in the rock layers to form a waterfall.
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Following a River from Source to Mouth
As the river continues, you will also find many tributaries – this is where one stream empties into another As more tributaries add water to the main river, the amount of discharge increases
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Tributaries
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Following a River from Source to Mouth
As the river moves downhill, it will erode its channel until it hits base level Base level is the lowest point to which a river can erode its channel.
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Following a River from Source to Mouth
As a river approaches base level, it can develop meanders – bends in the stream channel
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Following a River from Source to Mouth
Delta - a fan-shaped sediment deposit where a river empties into an ocean at the mouth
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Lena River Delta in Siberia
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New Orleans: Built on Mississippi River Delta
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Meanders can turn into Oxbow lakes…here’s how
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Ox Bow Lakes Neck of meander is gradually eroded
Once cut off, the water takes the quickest/shortest route What’s left behind is the Ox Bow lake
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Sediment Transport in Rivers
Rivers & Streams carry sediment in 3 ways: In solution (dissolved load) In suspension (suspended load) Scooting or rolling along bottom (bed load)
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1. Dissolved Load Sediments that are dissolved in river water
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2. Suspended Load Fine-grained sediment (like sand, silt, clay) that remains in the water during transportation Usually what you see that makes a river look dirty Most sediment carried by a stream is suspended This amount increases dramatically during floods
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3. Bed Load Heavier, coarse grained sediments that travel along the bottom of a stream. Causes the most stream erosion! Sediment may not move frequently
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Over 55% of U.S. rivers and streams are so polluted that they are no longer safe for fish and other aquatic life!!
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Quiz Vocabulary Stream Velocity Gradient Discharge Stream Channel
Source/Headwaters Alluvial Fan Tributaries Base Level Meander Delta Ox Bow Lake Dissolved Load Suspended Load Bed Load
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