Levees
Levees are natural embankments which are formed when a river floods. When a river floods friction with the floodplain leads to a rapid decrease in the velocity of the river and therefore its capacity to transport material. Larger material is deposited closest to the river bank. This often leads to large, raised mounds being formed. Smaller material is deposited further away and leads to the formation of gently sloping sides of the levees. High pressure, caused by a river meeting its bank-full capacity, can cause a levee to burst.
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Drainage basin hydrological cycle
Find out about the characteristics of the drainage basing hydrological cycle.
Storm Hydrograph
Hydrographs can be used to illustrate discharge. These can be used to show annual discharge patters of flow in relation to climate.
The long profile of a river
The long profile of a river shows changes in the height (altitude) of the course of a river from its source to its mouth.
Water Balance
The balance between inputs and outputs is known as the water balance or budget. The water…
Erosion, transportation and deposition
There are three main types of processes that occur in a river. These are erosion, transportation and deposition.
Changing channel characteristics
The characteristics of a river channel change along its long profile. Changes occur in the cross profile, wetted…