A meander is a winding curve or bend in a river. Meanders are the result of both erosional and depositional processes. They are typical of the middle and lower course of a river. This is because vertical erosion is replaced by a sideways form of erosion called LATERAL erosion, plus deposition within the floodplain.
The image below shows a series of meanders. Notice the deposition on the inside of the meanders (pale material) and the river cliffs or bluffs (indicated by dark shadows) on the outside of the meanders.
Again, the image below shows a series of meanders. The river shown in the photograph is swollen due to recent rainfall. Once again we can see deposition on the inside curves of the meander.
Erosion, transportation and deposition are all processes that create the characteristic features of meanders shown in the images above.
The videos below shows meander initiation and braiding in a small river model.
There are several stages involved in the creation of meanders. These are discussed below.
In low flow conditions straight river channels have bars of sediment on their beds. Flowing water weavers around these bars of sediment. This creates deeper pathways where most of the water flows called pools and shallow areas where less water flows called riffles. This causes the river flow to swing from side to side.
The map below shows bars of sediment exposed due to the low level of water in the channel. Notice how the flow of water weaves around the sediment bars.
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Where the river swings towards the bank erosion causes undercutting. On the opposite side of the channel where the velocity is lower material is deposited. Therefore the river does not get any wider. The image below shows evidence of undercutting on the outer bank and deposition on the inner bank of the meander.
Continued erosion along the outer bank, as the result of hydraulic action and abrasion, creates a river cliff or bluff. A point bar forms on the inner bank. This is a gently sloping deposit of sand, gravel and pebbles. The image below shows a point bar.
Meanders are perpetuated through a process called helicoidal flow. As the surface flow of water hits the outer bank it corkscrews, flows along the river bed then deposits eroded material on the inner bank.
Erosion is greatest beyond the middle of the bend in the meander. This causes the meander to migrate downstream over time. By looking at aerial photographs it is possible to see former channels on the floodplain.
The Drainage Basin Hydrological Cycle
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Question 1 of 7
1. Question1 points
Drainage basins are local, open systems. True or false?Correct
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What is the name of an area of land drained by a river and its tributaries?Correct
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What is the imaginary line separating drainage basins called?Correct
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Which of the following are not examples of inputs into the drainage basin hydrological cycle?Correct
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Which of the following is not an output from the drainage basin hydrological cycle?Correct
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Which of the following are examples of stores in the drainage basin hydrological cycle?Correct
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Which of the following are examples of transfers and flows in the drainage basin hydrological cycle?Correct
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