River landforms Flashcards
1
Q
How is a V-shaped valley formed?
A
- Rivers begin high up in the mountains so they flow quickly downhill eroding the landscape vertically.
- The river cuts a deep notch down into the landscape using hydraulic action, corrasion and corrosion.
- As the river erodes downwards the sides of the valley are exposed to weathering which loosens the rocks (some of which will fall into the river) and steepens the valley sides.
- The rocks which have fallen into the river help the process of abrasion and this leads to further erosion.
- The river transports the rocks downstream and the channel becomes wider and deeper creating a V-shaped valley between interlocking spurs.
2
Q
How do rapids form?
A
- Alternating bands of hard and soft rock
- The soft rock erodes faster than the hard rock.
- This cause the river bed to drop and create turbulent water
3
Q
How does a waterfall form?
A
- The river flows over bands of softer and harder rocks.
- Softer rock is more quickly eroded.
- The river undercuts the harder rock leaving an overhang.
- The river forms a plunge pool below the waterfall using hydraulic action, abrasion and corrosion.
- Overhanging rock is unsupported and falls into the plunge pool, abrasion is increased because of the material, attrition also takes place as the fallen rocks erode.
- The waterfall is moved upstream.
- This process continues and a gorge is cut back into the hillside.
4
Q
How does a meander form?
A
- Water twists and turns around stones and other obstructions resulting in areas of slower and faster water movement.
- The river starts to flow from side to side in a winding course but still in a relatively straight channel- helical flow.
- Water moving faster has more energy to erode (hydraulic action, corrosion). This occurs on the outside of the bend and forms a river cliff.
- The river erodes the outside bends through abrasion, corrosion and hydraulic action.
- Water moves slowly on the inside of the bend and the river deposits some load, forming a river beach/slip-off slope.
- Continuous erosion on the outer bank and deposition on the inner bank forms a meander in the river.
- The meander will migrate downstream and change shape over time.
5
Q
How does an ox-bow lake form?
A
- The river is meandering across the valley.
- The river is eroding laterally (from side to side).
- The river flows faster on the outside bends and erodes them.
- The river flows slowly on the inside bends and deposits material so its course is changing.
- Continual erosion and deposition narrows the neck of the meander.
- Often during a flood the river will cut through the neck.
- The river continues on its straighter path and the meander is abandoned.
- New deposition seals off the ends and the cut-off becomes an oxbow lake that will eventually dry up.
6
Q
How does a levee form?
A
- The river is on its floodplain with a very low gradient.
- The river is mainly depositing (silt and sand).
- When the river floods a lot of silt is deposited on the river banks and much less on the floodplain.
- Frequent flooding continues this build up.
- When the river is flowing normally it deposits in the river bed.
- This raises the river above the floodplain.
- Usually the built-up levées protect the plain from flooding.
7
Q
How does a floodplain form?
A
- The Flood Plain is the area of alluvial deposits found beside the river in its lower course (often used for agriculture).
- As meanders move slowly down the course of the river they erode away the valley to create a wide valley floor, and they deposit layers of alluvial material on the slip off slopes.
8
Q
How do deltas form?
A
- Deltas occur where a river that carries a large amount of sediment meets a lake or the sea.
- This meeting causes the river to lose energy and drop the sediment it is carrying.
- An example is the Nile Delta in Egypt.
9
Q
What are the 2 different types of delta?
A
- Bird’s foot delta: the flow of the river is stronger than the sea, so the distributaries carry the sediment out into the sea. eg. the Mississippi delta
- Arcuate delta: shaped like a fan. When the sea has a strong current, and the sediment is kept close to the coast. eg. the Zambezi delta
10
Q
Niagara Falls
A
- Length of brink: 2600 ft
- Height: 167 ft
- Volume of water: 6 million cubic feet per minute in peak flow
- Hard rock of resistant Limestone. Underneath layers of softer Shale and Sandstone
- The falls have a Headward Erosion rate of 1 metre per year.
- Niagara has a deep gorge, over 11 km in length.
- Two power stations (HEP) run off the tremendous power of the River Niagara’s flow.
- The Horseshoe Falls are Canadian but 1/3 of the Falls actually lies in US territory
- The falls lie 120km south-east of Toronto, Canada. They are 27km north-northwest of Buffalo, New York.
- Niagara Falls consists of 3 major waterfalls, The Horseshoe, The American Falls and the smaller Bridal Vail Falls