Landforms & channel types along a river's course
- Created by: Max Oscar
- Created on: 16-04-22 12:28
A river runs from source along its course to the mouth of the river
What is a river's course? Different stages of a river
What is the mouth of the river? Where the river gets to the sea
What is the source of a river? The start of a river
There are 4 main parts to a river's course:
- Upper course
- Middle course
- Lower course
- Mouth
Landforms are found at different stages of a river's course:
Upper course (steep v-shape downward erosion):
- Rapids
- V-shaped valley
- Waterfalls
- Interlocking Spurs
Middle course (u-shaped lateral erosion):
- Meanders
- U-shaped valley
- Oxbow lakes
Lower course (open/wide u-shape lateral erosion & deposition):
- Wide Floodplains
- Estuaries
- Levees
- Deltas
Landforms are produced by erosion, transport & deposition of rivers
KEY River landforms:
- Braided channels
- Rapids & Waterfalls
- Meanders & Oxbow lakes
- Floodplains
- Levees
- Deltas
Landforms are made by natural processes and can be seen on Earth's surface (e.g. meanders)
Braided channels
Braiding occurs when a river does not have the capacity to transport it's load in a single channel so deposits it in short term, temporary bars (eyots) or long term vegetated islands
A river may lose its capacity when:
- Discharge is reduced (e.g. Following a period of low rainfall)
- When they are shallow areas in river
Banks are easily erodible meaning river is heavily laden with sediment
Example of Braided River: Brahmaputra River, Bangladesh
- A very large braided river
- Sediment is deposited during snowmelt from the Himalayas in the spring time, which is then shaped into eyots & during remainder of the year
Waterfalls
Waterfall = cascade of water falling from a height, formed when river falls off precipice/steep incline
- Waterfalls occur when river flows over rocks of differing resistance
- Harder more resistant rocks resist erosion but soft less resistant rocks erode quickly (differential erosion)
Mini case study: High Force, River Tees, UK
- Located on River Tees in the UK
- 20m in height
- Formed where River Tees crosses whin sill (a hard layer of rock)
- Underlying the whin sill is a layer of carboniferous limestone (a softer rock) which is easily worn away by waterfall
- As limestone is eroded the whin sill is left overhanging the waterfall.
- Overhang eventually collapses
- As this process repeats, waterfall takes shape & retreats leaving a narrow, deep gorge in front of it.
Gorges
Gorge = narrow & deep section of a river valley with vertical/near-vertical valley sides
- Gorges are most commonly formed as a result of waterfall retreat (e.g. the 700m gorge in front of High Force waterfall, UK)
They can also be formed by:
- Movement and melting of glaciers which cut deep Valleys in the earth's surface
- Surface runoff over limestone during Ice Age (water within limestone froze, making it impermeable)
- During spring snowmelt, water remains over impermeable limestone, forming a gorge (e.g. Cheddar Gorge)
Meanders
Meander…
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