Grinding of rock fragments carried by a river against the bed and banks of that river. This action causes the river channel to widen and deepen. This grinding is most powerful during a flood
Solution
Process by which river water dissolves minerals in rocks and chemically reacts with soluble minerals
Hydraulic action
Form of mechanical weathering caused by the force of moving water, which can force air into cracks and undermine or erode the outside of a river bank, especially in waterfalls
Transportation
The movement of material by rivers, which need energy to transport material and levels of energy change from the source to the mouth of the river
Deposition
The laying down of material previously transported by a river when the velocity of the river is reduced, causing the river to drop its load
The river has more energy to transport material by Suspension
This material Beats the Queside bank by Corros fabrauts
The bank will be undercut, Calinese and retreut leaving a Small River cliff
On the inside bend there is an increase in friction and a decrease in velocity
Inside bend Characteristics
Reduction in friction
Increase in velocity
Increase in erosion
Outside bend Characteristics
Fastest flow
Reach fat
Ba lum
Reduction in friction, increase in velocity, increase in cangy, increase in erosion when bank is undercut
Flood plains
The area of land on either side of a river which is flooded during times of flood
At times of high discharge the river has a long way to transport material by Suspension
Each time a river floods, a layer of sediment is deposited
The coarsest/smallest drop first close to the bank to form a levee
The fine material deposited on the floodplain increases the fertility of the soil
Impacts of flooding on people and environment
People and animals can become homeless
Buildings can be damaged or destroyed
Crops can be lost
Positive - Replenishes drinking water
Provides sediment
Fish benefit as they feed on insects washed in
Can encourage innovative solutions
Wild animals may drown or lose their habitat
Flood management includes hard engineering methods and soft engineering methods
Hard engineering methods are not sustainable
Soft engineering methods
Afforestation
Land use Zoning
Wash lands
The hydrological cycle is the continual transfer of water between the land, sea, and atmosphere
Definitions related to rivers
Drainage Basin: An area of land drained by a river and all its tributaries
Tributary: A stream which flows into a larger river
Watershed: Boundary between drainage basins, often a ridge or high bank
River Channel: Where the tributaries meet
Source: The starting point of a river
Confluence: The point where two rivers meet
Mouth: The end of a river where it flows into the sea or lake
Precipitation: Any form of water falling from the sky
Surface runoff: Water moving over the land surface
Through-flow: Water flowing through the soil
Percolation: Water sinking down through the soil
Groundwater flow: Water flowing slowly underground
River discharge: Water flowing out early in the river to the sea or lake
Evaporation: The transfer of water from the sea to the air
Vapour: Water in the form of gas
Long Profiles of rivers may be directed upstream or downstream
Long Profiles are concave in shape but different rock types make them irregular
Bradshaw model: Shows how characteristics of rivers change along their course
Interlocking Spurs: Energy used to transport large boulders along the river bed through vertical erosion
River downstream towards the mouth flows over flatter land and develops large bends called meanders
Lateral erosion occurs in the middle course of the river