River landscapes and processes Flashcards
What are the three courses of a river?
- Upper course
- Middle course
- Lower course
Characteristics of upper course?
- Steep gradient
- V-shaped valley
- Steep sides
- Narrow, shallow channel
Characteristics of middle course?
- Medium gradient
- Gently-sloping valley sides
- Wider, deeper channel
Characteristics of lower course?
- Gentle gradient
- Very wide, almost flat valley
- Very wide, deep channel
What is the long profile of a river?
- Shows you how the gradient changes over the different courses.
What is the cross profile of a river?
- Shows you what a cross section of the river looks like.
How does verticle erosion alter the cross profile of a river?
- Verticle erosion deepens the river valley and channel, making it v-shaped.
- Verticle erosion is dominant in the upper course of a river.
- High turbulence causes the rough, angular particles to be scraped along the river bed, causing intense downward erosion.
How does latural erosion alter the cross profile of a river.
- This widens the river valley and channel during the formation of meanders.
- It is dominant in the middle and lower courses.
Why is the upper course the way it is?
- The valley is steep-sided due to verticle erosion and the channel has a steep gradient.
- The river channel is narrow and shallow - this means discharge is low. The velocity is low due to friction from the rough channel sides and bed.
- The river carried large, angular stones.
Why is the middle course the way it is?
- The river valley becomes wider due to lateral erosion.
- The valley sides become gentle slopes and the gradient of the channel is less steep.
- The river channel becomes wider and deeper.
- Discharge increases as more streams join the river.
- The river has a higher velocity as the channel sides are smoother, which leads to less friction.
- The river’s sediment load is made up of smaller and more rounded rocks as erosion continues.
Why is the lower course the way it is?
- In the lower course, the valley is very wide and flat.
- The river has a high velocity because there is very little friction from the channel’s smooth sides.
- It has a large discharge due to more tributaries joining it.
- The river channel is very wide and deep.
Difference between slides and slumps?
- In slides, material shifts in a straight line.
- In slumps, material shifts with a rotation.
How does geology influence river landforms?
- Rivers flowing through areas of hard rock have a slower rate of erosion because hard rocks are more resistant, whereas areas with softer rocks will experience more erosion.
- Landscapes with more resistant rocks tend to have steeper valley sides, landscapes with less resistant rocks tend to have gentle sloping valley sides.
How is a waterfall formed?
- Waterfalls form where a river flows over an area of hard rock followed by an area of softer rock.
- The softer rock is eroded by hydraulic action and abrasion more than the hard rock, creating a ‘step’ in the river.
- As water goes over the step it erodes more and more of the softer rock.
- A steep drop is eventually created, which is called a waterfall.
- The hard rock is eventually undercut by erosion. It becomes unsupported and collapses.
- The collapsed rocks are swirled around at the foot of the waterfall where they erode the softer rock by abrasion. This creates a deep plunge pool.
How is a gorge formed from a waterfall?
- Over time, more undercutting causes more collapses. The waterfall will retreat and leave behind a steep-sided gorge.
How are interlocking spurs formed?
- In the upper course of a river most of the erosion is vertically downwards. This creates steep sided V-shaped valleys.
- The rivers aren’t powerful enough to erode laterally - they have to wind around the spurs that stick out into their paths on either side.
- These hillsides are often made of a resistant rock which the river can’t erode, so the river erodes the less resistant rock between the spurs as it winds down the valley.
- The hillsides that interlock with each other as the river winds around them are called interlocking spurs.
What is deposition?
- Deposition is when a river drops eroded material
- It happens when a river slows down
What are meanders?
- Rivers develop large bends called meanders in their middle and lower course, in areas where there are both shallow and deep sections in the channel.
How are meanders formed?
- The current is faster on the outside of the bend because the river channel is deeper. (Less friction to slow the water down)
- So the outside of the bend is a high-energy environment, meaning more erosion take splace there, forming steep sided river cliffs.
- The inside of the bend is a low energy environment. The current is slower there because the river channel is shallower (more friction)
- So eroded material is deposited on the inside of the bend.
- Over time, this material builds up to form a point bar - a crescent shaped gentle slope made of sand or stones.
How are ox-bow lakes formed?
- Erosion caused the outside bends to get closer.
- Eventually there’s only a small bit of land left between the bends called the neck.
- The river breaks through this land, usually during a flood.
- The river continues to flow along the shortest course.
- Deposition eventually cuts off the meander.
- This forms an ox-bow lake.
What is a flood plain?
- Thr flood plain is the wide valley floor on either side of a river which occasionally gets flooded.
How is a flood plain made?
- river floods onto the flood plain, the water slows down and deposits the eroded material that it’s transporting –> builds up flood plain
- Meanders migrate across the flood plain, making it wider
- Meanders also migrate downstream, flattening out the valley floo
- Deposition that happens on the point bars of meanders -> builds up the flood plain.
How are leeves formed?
- Leeves are natural embankments along the edges of a river channel
- During flood, eroded material deposited over whole flood plain
- Heaviest material deposited closest to river channel because its dropped first when river slows down
- Over time the deposited material builds up creating leeves along the edges of the channel.
How does climate (rainfall) influence river landscapes?
- higher discharge –> more water entering the channel
- Higher discharge increases the rate of erosion - higher volume of water -> more power to erode river banks and beds -> adds material to the rivers load.
- Shapes the landscape - forms V-shaped valleys in river’s upper course and wide, flat flood plain in the lower course
- Transporation increases when river has higher discharge because more energy to carry material
- Chemical weathering increases -> Carbonation and dissolution weathering can happen when rainwater comes into contact with minerals that make up the rocks in the river valley -> valley sides more unstable