Comp 2 Topic 4 - River Processes And Pressures Flashcards
(59 cards)
What is the path of a river called as it flows downhill?
Its course
What are the different courses of a river?
Upper course (closest to the source of the river) Middle course ( in the middle) Lower course (closest to the mouth of the river)
What does the shape of the valley or channel tell you about the river?
Whether the river is eroding more or depositing more sediment.
What is the long profile?
Shows you how the gradient changes over the course
What is the cross profile of a river?
Shows you what the cross section of a river looks like
What are the characteristics of a river in the upper course?
The gradient is steep
V-shaped valley, steep sides, narrow, shallow channel
What are the characteristics of a river in the middle course?
The gradient is medium
Gentle sloping valley sides, wider, deeper channel
What are the characteristics of a river in the lower course?
The gradient is gentle
Very wide, almost flat valley very wide, deep channel
What is vertical erosion and where does it happen most frequently?
It deepens the river valley and channel making it V shaped.
It happens most frequently in the upper course of the river.
High turbulence causes rough pieces of rock and sediment to scrape the bottom of the river bed causing intense downward erosion
What is lateral erosion and where does it happen most frequently?
This widens the river valley and channel During the formation of meanders
Its dominant in the lower and middle courses
Describe the river Eden’s upper course
- The source is 600m above sea level in an area of hard, resistant rock.
- The valley is steep sided due to vertical erosion, the channel has a steep gradient.
- The river channel is narrow and shallow, meaning discharge is slow. The velocity is low due to the rough channel sides and bed.
- The river carries large angular stones.
Describe the river Eden’s middle course
- The middle parts of the river are made from sandstone which is easily eroded, it means that the river is wide due to lateral erosion.
- The gradient and sides of the river are less steep
- the river channel also becomes wider and deeper
- Discharge increases as more streams join the main river (tributaries)
- The river has smaller rounder rocks through erosion
Describe the river Eden’s lower course
- In the lower course the valley is very wide and flat
- By the time the river reaches carlisle it is only a few meters above sea level
- The river has a high velocity because theres very little friction from the channels smooth sides
- It has a very large discharge because two other rivers join the eden
- The river in carlisle is nearly 50m wide, very wide and deep
- material carried by the river is very fine and well rounded
How does weathering shape river valleys?
Weathering breaks down rock on valley sides.
Freeze thaw happens when temperature fluctuates above and below zero degrees c
Repeated freeze thawing widens rivers by breaking the sides down
What are the 4 types of erosion and what do they do?
Hydralic action- the force of the water breaks rock particles away from the river channel.
Abrasion- eroded rocks scrape the sides and bed of the river, this is the most common form of erosion
Attrition- eroded rocks picked up by the river smash into each other and break into smaller fragments. Their edges get rounded off as they rub together. Attrition causes particle size to decrease in the course.
Solution- river water dissolves some types of rock (chalk and limestone)
What are the 4 types of transportation?
Traction
Saltation
Suspension
Solution
What is traction?
Large particles like boulders are pushed along the river bed by the force of the water
What is saltation?
Pebble sized particles are bounced along the river bed by the force of the water
What is suspension?
Small particles like silt and clay are carried along by the water
What is solution?
Soluble materials dissolve in water and are carried along
What is deposition?
It is when the river drops eroded material it is carrying, It happens when the velocity of a river reduces.
The reasons this could happen include:
-The volume of water in the river falls
-The amount of eroded material in the river increases
-The water is shallower
-The river reaches its mouth
How are waterfalls and gorged formed?
1) They are formed where are river flows from an area of hard to soft rock
2) The softer rock is eroded ore than hard rock creating a step in the river
3) The step gets bigger through repeated erosion
4) A steep drop is eventually created
5) The hard rock is eventually undercut, becomes unsupported and collapses
6) The collapsed rocks are swirled around at the foot of the waterfall where they erode the softer rocks by abrasion, it creates a deep plunge pool
7) Over time more undercutting causes more collapses, the waterfall will retreat leaving behind a steep sided gorge
What are interlocking spurs?
In the upper course most erosion is lateral creating steep v shaped valleys
The rivers don’t have enough power to erode laterally so they wind around hills that stick out in their way
The hillsides that interlock as the river flows between them are called interlocking spurs
How are meanders formed?
Rivers develop meanders in the middle and lower course in areas of deep and shallow water.
1) The current is faster on the outside of the bend because the river channel is deeper (less friction)
2) More erosion (abrasion and hydraulic) take place on the outsides forming river cliffs
3) The current is slower on the inside of the bend because the river channel is shallower (more friction)
4) Eroded material is deposited on the inside bend forming slip off slopes.