Rivers Flashcards

1
Q

Dams

A

Dams + reservoirs. Dams are barriers and reservoirs are artificial lakes. Reservoirs store water and generate Hydroelectric power. Dams are expensive, creating a reservoir can flood existing settlements. Farmland downstream can become less fertile.

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2
Q

Channel Straightening

A

Meanders are removed by buildings straight, artificial channels. Water leaves the area quickly, so flood risk is lower. Flooding can happen downstream though, faster moving water can cause more erosion downstream.

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3
Q

Embankments

A

Raised walls are built along river banks. The river can hold more water, so floods are less frequent. They’re expensive, and a risk of flooding if water level rises.

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4
Q

Flood relief channels

A

Channels built to divert water around built-up areas or to divert excess water if the river level gets too high. Gates on the channels mean that the release of water can be controlled, reducing flood risk. There will be increased discharge where the relief channel rejoins the river, which could cause flooding in that area

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5
Q

Flood warnings and preparation

A

Give people time to move possessions. But don’t actually prevent floods.

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6
Q

Flood plain zoning

A

Planting trees in river valley increases interception of rainwater. Discharge and flood risk decrease. Vegetation reduces soil erosion in the valley and provides habitats for wildlife. Less land available for farming.

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7
Q

River restoration

A

Making river more natural, removing man made levees for example. Discharge is reduced, Less chance of flooding downstream. Little maintenance is needed and there are better habitats for wildlife. Local flood risk can increase especially if nothing is done to prevent major flooding

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8
Q

Upper Course of a River has:

A
  • Steep Gradient
  • V-Shaped Valley
  • Steep Sides
  • Narrow, shallow channel
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9
Q

Middle course of a river has:

A
  • Medium Gradient
  • Gently sloping valley dies
  • Wider, deeper channel
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10
Q

Lower course of a river has:

A
  • Gentle gradient
  • Very wide, almost flat valley
  • Very wide, deep channel.
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11
Q

Vertical Erosion:

A
  • Deepens the river valley and channel, making it V-Shaped.
  • Happens in the upper course
  • High turbulence causes the rough, angular particles to be scraped along the river bed, causing intense downwards erosion.
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12
Q

Lateral Erosion:

A
  • Widens the river valley and channel during the formation of meanders.
  • Dominant in middle and lower courses of a river.
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13
Q

Hydraulic Action:

A
  • The force of the river weather colliding with rocks breaks rock particles away from the river channel.
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14
Q

Abrasion:

A
  • Eroded rocks picked up by the river scrape and rub against the channel, wearing it away.
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15
Q

Attrition:

A
  • Eroded rocks picked up by the river crash into each other and break into smaller fragments.
  • Their edges get rounded off as they rub together.
  • The further material travels, the more it is eroded - attrition causes particle size to decrease from a river’s source to its mouth.
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16
Q

Solution (erosion):

A
  • River Water dissolves some types of rock like chalk and limestone.
17
Q

Traction:

A
  • Large particles like boulders are pushed along the river bed by the force of the water.
18
Q

Saltation:

A
  • Pebble-sized particles are bounced along the river bed by the force of the water.
19
Q

Suspension:

A
  • Small particles like silt and clay are carried along by the water.
20
Q

Solution (transportation):

A
  • Soluble materials like limestone dissolve in the water and are carried along.
21
Q

When does deposition occur?

A
  • When a river loses velocity and energy.
22
Q

Why do rivers slow down and deposit material?

A
  • Volume of water falls
  • Amount of eroded material increases
  • River is shallower e.g on inside of a bend
  • River reaches its mouth
23
Q

How does particle size affect how far material is transported?

A
  • Smaller particles are transported further and deposited closer to the river’s mouth.
24
Q

How do waterfalls form? (6 marks)

A
  • They 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 flows over the step it erodes more and more of the softer rock.
  • A steep drop is eventually eroded, 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.
  • Over time, more undercutting causes more collapses. The waterfall retreats, leaving behind a steep-sided gorge.
25
Q

What are interlocking spurs?

A
  • The hillsides that interlock with each other as the river winds around them.
26
Q

How do interlocking spurs form?

A
  • In the upper course, most erosion is vertically downwards which creates steep-sided, v-shaped valleys.
  • The rivers lack the power to erode laterally, so they have to wind around the high hillsides that stick out into their paths on either side.
27
Q

How do meanders form?

A
  • The current is faster on the outside bend because the river channel is deeper.
  • More erosion takes place on the outside bend, forming river cliffs.
  • The current is slower on the inside bend because the river channel is shallower.
  • So eroded material is deposited on the inside of the bend, forming slip-off slopes.
28
Q

What is the thalweg?

A
  • The line of deepest water and fastest flow in a river channel.
29
Q

How do meanders form ox-bow lakes?

A
  • Erosion causes the outside bends to get closer until there’s only a small bit of lands left between the bands called the neck.
  • The river breaks through this land, usually during a flood and the river flows along the shortest course.
  • Deposition eventually cuts off the meander forming an ox-bow lake.
30
Q

What is the flood plain?

A
  • The wide valley floor on either side of a river which occasionally floods.
31
Q

How do flood plains form?

A
  • When rivers flood, the water slows down, loses energy and deposits the material that it’s transporting. This builds up the flood plain.
  • Meanders widen as they migrate across floodplains laterally.
  • Over time, meanders also migrate downstream.
  • The deposition that happens on the slip-off slopes of meanders also builds up the flood plain.
32
Q

What are levees?

A
  • Natural embankments (raised banks) along the edges of a river channel.
33
Q

How do levees form?

A
  • During a flood, eroded material is deposited over the whole flood plain.
  • The heaviest material is deposited closest to the river channel, because it gets dropped first when the river slows down and loses energy.
  • Over time, the deposited material builds up, creating levees along the edges of the channel.
34
Q

What are estuaries?

A
  • Tidal areas where the river meets the sea.
35
Q

How do estuaries form?

A
  • The river valley it at its widest at the river mouth and the land is close to sea level.
  • The water is tidal (rises and falls each day).
  • When the water floods over the banks of a river, it carries silt and sand onto the valley floor.
  • As the tide reaches its highest point, the water moves slowly and his little energy, so it deposits sediment.
  • Over time, more mud build up, creating large mudflats.
  • At low tide, the wide, muddy banks are exposed.
36
Q

Upper Course Evidence:

A
  • Waterfalls
  • Symbol for a cliff (black, blocky lines)
  • High lands
  • Crosses lots of contour lines in a short distance (steep)
  • Narrow (thin, blue line)
  • Close contour lines and the valley floor is narrow (river is in a steep-sided, V-shaped valley).
37
Q

Lower course evidence:

A
  • Low
  • Doesn’t cross any contour lines so it’s very gently sloping
  • River meanders across a large, flat area, which is the flood plain.
  • Wide (thick, blue line)
  • Large meanders (ox-bow lake may form here).