Rivers Flashcards
types of erosion
abrasion
hydraulic action
attrition
solution
hydraulic action
the sheer power of the waves as they smash against the cliff. air becomes trapped in the cracks in the rock and causes the rock to break apart from the pressure.
attrition
rocks in the water knock against each other. they break apart to become smaller and rounder
abrasion
pebbles grind along a rock platform, like sandpaper. over time, the rock becomes smooth
solution (erosion)
sea water dissolves certain types of rocks and breaks down some rock. in the UK, chalk and limestone cliffs are prone to this.
types of transportation
traction
saltation
solution
suspension
traction
where pebbles and larger material are rolled along the seabed
saltation
where small pieces of shingle or large sand grains are bounced along the sea bed
suspension
small particles such as silts and clays are suspended in the flow of the water
solution (transportation)
when materials in rocks like chalk and limestone are dissolved in sea water and then carried in solution. the load is not visible
characteristics of the upper course
steep gradient
V-shaped valley, steep sides.
Narrow, shallow channel
Bedload is large and angular
Lots of vertical erosion
low velocity
small discharge
characteristics of the middle course
medium gradient
Gently sloping valley sides. Wider, deeper
channel
Load becomes smaller and less angular.
Lateral erosion increases
characteristics of the lower course
gentle gradient
Very wide, almost flat valley, very wide, deep
channel
Large amount of load but the size is small and
very rounded. A lot of lateral erosion occurs
high velocity
large discharge
formation of meanders
- In the middle course, the river has more energy and the land is flatter. This causes the river to meander and more lateral
erosion occurs. There is a disturbance making a hole in one bank. Water flows into it and erodes it, beginning a bend. - Water flows faster on the outside bend, eroding it creating a river cliff.
- Material is deposited in the slow moving water on the inside bend creating a slip-off slope
- over time the amplitude of the bend increases making the meander more pronounced
formation of oxbow lakes
- Oxbow lakes begin with a meander.
2 . The water on the inside of the bend is moving slowly and has less energy, so material is deposited here. - Water flows faster on the outside bends eroding them so that they get closer together.
- Gradually over time, two outside bends can erode so much that the meander neck narrows until they touch and during a time of flood, the water can break through the land between them. The river takes the straighter, faster route so less water flows around the bend
- Material is deposited in the slow moving water in the old bend, cutting if off and creating an ox-bow lake.
formation of a v-shaped valley
- Water collects on high ground after heavy rain and begins to flow downhill because of gravity. Gradually, the river erodes the underlying rock creating a channel.
- The sides of the channel are exposed to the weather. Weathering breaks up the rocks on the valley sides.
- The weathered rock on the valley sides falls into the river channel (mass movement). some is carried away by the river
- the process repeats, and the v-shaped valley becomes deeper.
features of the upper course
waterfalls
v-shaped valleys
inter-locking spurs
features of the middle course
meanders
features of the lower course
meanders
ox-bow lakes
floodplains
levees
physical causes of river flooding
antecedent rainfall
impermeable rock
relief
weather conditions
human causes of river flooding
urbanisation
agriculture
deforestation
climate change
causes of river flooding: urbanisation
surfaces like roads are impermeable»_space; more surface run-off»_space; water returns to the river faster increasing the risk of flooding. rainwater also flows into drains which returns water to the river faster
causes of river flooding: agriculture
irrigation up and down (instead of across) hillsides creates channels»_space; allows water to reach rivers faster»_space; increasing discharge
causes of river flooding: deforestation
less interception»_space; rain reaches the ground faster»_space; ground is more likely to become saturated»_space; more surface run-off»_space; water returns to the river faster increasing discharge