List characteristics of the drainage basin
Source
Watershed
Confluence
Tributary
Mouth
What is an open system and give an example
The amount of water can vary, as it has inputs and outputs
Eg: Drainage basin
List inputs
Precipitation
List stores
Interception
Soil moisture
Surface storage
Ground water
List flows/transfers
Infiltration
Percolation
Groundwater flow
Through flow
Surface run off
List outputs
Evaporation
Evapotranspiration
River carrying water to a lake or sea
Upper course: channel characteristics
Narrow, shallow channel with a steep gradient and uneven bank
Middle course: channel characteristics
Channel widens due to lateral erosion
Lower course: channel characteristics
Wide and deep channel with a shallow gradient and smooth banks
Upper course: type of erosion
Vertical erosion
Middle course: type of erosion
Lateral erosion
And deposition seen on meanders
Lower course: type of erosion
Lateral erosion but deposition is more common here
Upper course: type of transport
By saltation and traction
Middle course: type of transport
All methods of transport can be seen but most common is suspension
Lower course: type of transport
Load moved by suspension
Upper course: size of load
Large angular boulders
Middle course: side of load
Load becomes smaller and more rounded
Lower course: size of load
Small rounded pebbles
List the conditions when deposition is likely to occur
How does deposition work
When the velocity of the river is reduced, the energy of the water decreases, and so the water can no longer erode or transport material. Instead, the load is dropped, starting with the largest (and heaviest) particles.
What’s the Bradshaw model
A theoretical geographical model that helps describe how a rivers characteristics vary between upper and lower course of a river
How are water falls formed
-There is a layer of hard rock over a layer of softer rock
-the softer rock is more easily eroded, so the hard rock is undercut
-a step is formed but the process of abrasion and hydraulic action
-the river falls into a plunge pool and eventually the overhanging hard rock will collapse due to this undercutting
-finally the waterfall retreats backwards/upstream forming a gorge
How are levees formed
-a river overflows its banks, the velocity decreases
- this causes energy to decrease and the river must depositor much of its load into the floodplain
- the largest load is deposited first
-over time after repeated floods, layers of deposited material builds up to form natural embankments called levees
- levees can be artificially strengthened and raised to protect floodplain from flooding
What are the positive impacts of flooding on people
-Replenishes drinking water supply
-can encourage innovative solutions in future building design
-provides sediment that naturally fertilisers the soil of the floodplain
-countries such as Bangladesh and Egypt rely on floods to help crops (like rice) grow