river landscapes 1 ✓ Flashcards
what does the river valley look like in the upper course ?
- steep gradient
- v-shaped valley
- steep sides
- narrow, shallow channel
what does the river valley look like in the middle course ?
- medium gradient
- gently sloping valley sides
- wider deeper channel
what does the river valley look like in the lower course ?
- gentle gradient
- very wide
- almost flat valley
- very wide and deep channel
how does the width of a river change from source to mouth ?
gets wider
how does the depth of a river change from source to mouth ?
gets deeper
how does the gradient of a river change from source to mouth ?
gets flatter
how does the discharge of a river change from source to mouth ?
size of discharge gets larger
how does the velocity of a river change from source to mouth ?
gets faster
how does the sediment size of a river change from source to mouth ?
gets smaller
how does the sediment shape of a river change from source to mouth ?
gets more rounded
what is the structure of sedimentary rock ?
- in layers
- made from animals remains
- easily eroded
- soft rock
how does the structure of sedimentary rock affect the way and speed it erodes ?
- more easily eroded
- layers are reasonably easy to erode
how do storms affect the rate of erosion ?
- increase rate of erosion
- winds make waves stronger
- increased water increases velocity
how does the rate of erosion differ in summer than in winter ?
- rains less in summer
- hotter in summer
- in winter rains more which means more water added into the rivers and the sea increasing velocity of water increasing rate of erosion
how does erosion create interlocking spurs ?
- upper course there is more vertical erosion
- river cuts down into the valley
- if there are areas of hard rock which are harder to erode, the river will bend around it
- this creates interlocking spurs
how does erosion create waterfalls ?
- layer of harder rock (whinstone) sits upon softer rock (carboniferous limestone)
- the limestone is easy to erode and is eroded away by hydraulic action creating a plunge pool
- as the notch grows the whinstone is left unsupported and falls into the water
- this constantly repeats creating a gorge and causing the waterfall to retread headwards
how does erosion create gorges ?
- layer of harder rock (whinstone) sits upon softer rock (carboniferous limestone)
- the limestone is easy to erode and is eroded away by hydraulic action creating a plunge pool
- as the notch grows the whinstone is left unsupported and falls into the water
- this constantly repeats creating a gorge
how does erosion create river cliffs ?
- a river goes around a bend, most of the water is pushed towards the outside
- causes increased speed and therefore increased erosion (through hydraulic action and abrasion).
- lateral erosion on the outside bend causes undercutting of the bank to form a river cliff
how does deposition create meanders ?
- river makes its way to the middle course, it gains more water and therefore more energy
- lateral erosion starts to widen the river
- when the river flows over flatter land they develop large bends called meanders
how does deposition create flood plains ?
- floodplains form due to both erosion and deposition
- erosion removes any interlocking spurs, creating a wide, flat area on either side of the river
- during a flood, material being carried by the river is deposited
- over time, the height of the floodplain increases as material is deposited on either side of the river
how does deposition create levees ?
- levees occur in the lower course of a river when there is an increase in the volume of water flowing downstream and flooding occurs
- sediment that has been eroded further upstream is transported downstream
- when the river floods, the sediment spreads out across the floodplain
- when a flood occurs, the river loses energy. The largest material is deposited first on the sides of the river banks and smaller material further away
- after many floods, the sediment builds up to increase the height of the river banks, channel can carry more water (a greater discharge) and flooding is less likely to occur in the future
how does deposition create a point bar (slip off slope) ?
the build up of deposited sediment in the inside of a meander bend is called a slip off slope
how has urbanisation affect rivers and river processes ?
natural river processes can be reduced because of engineering that stops the rivers from flooding this an change the natural shape of the river
how has agriculture affect rivers and river processes ?
- fertilisers and pesticides can contaminate the river
- land is taken up by agriculture and therefore protected by people to stop the river from flooding the area