A bank or levee is the raised portion of the floodplain next to the channel.
Water can exit a channel in 3 different ways.
Once bankful discharge is reached and exceeded, water spills out of the channel over top of the bank.
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Water exits the channel through a breach in the bank.
SEE PHOTO
Water exits the channel as groundwater because of the weight of the higher water in the channel pushing around.
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When water leaves the channel through a breach in the bank, it is an avulsion.
A Crevasse-splay.
A fan shaped deposit that is thicker and coarser near the breech changing to thinner and finer away from the channel.
The way to control a flood is to keep excess water in the channel, or if it won’t stay in the channel, a place for it to go.
3.
Structures, usually piles of sediment, on top of the river bank that raise the bank to create more room in the channel for water.
While these are cheap and effective, they do have drawbacks:
Sediment that would normally leave the channel during a flood remains there. This sediment will start to fill the channel, reducing its depth.
Levees can also make a flood worse because they can act as a barrier to the return of water into the channel.
Artificial channels intended to direct excess water back into the river.
They will take excess water and redirect around areas needing protection.
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Permafrost/frozen ground makes the ground impermeable.
Precipitation is therefore quickly channeled into the river adding to a faster increase in Q.
If there is flooding, this excess water will remain on the surface, making the flood worse.