Geography- Unit 1.2.1/ How do rivers change overtime? Flashcards

1
Q

Abrasion

A

The movement of rocks grinding against other rocks thus eroding them through a sandpaper like affect

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2
Q

Attrition

A

Rocks hitting each other and breaking apart into smaller rocks.

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3
Q

Hydraulic action

A

Rapid water movements with high energy hitting rocks/ other material and thus eroding it and pushing cracks in rocks

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4
Q

Solution

A

Certain rocks are dissolved in water e.g limestone.

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5
Q

Traction

A

Movement of large boulders rolling across the floor from water pushes.

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6
Q

Suspension

A

Smaller particles are held up in the water and moved down stream/ current/ tide.

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7
Q

Saltation

A

Smaller rocks hit the sides of the river, causing others to bounce of, thus creating a cycle.

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8
Q

Deposition

A

when a river loses energy and drops the material it carries.

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9
Q

fluvial erosion

A

Erosion that occurs in a river

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10
Q

Why does deposition occur?

A

-Decrease in velocity gradient
- Too much load (caused by landslides)
-Less water/ shallow water
-Too much water e.g floodplain.

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11
Q

What is the Hjulstrom curve?

A

-With higher velocity, more particles are eroded
- In water with less velocity and smaller particle sizes are transported
- Larger particles even with slightly high velocity are deposited
- Larger particles ( silt or other materials) are deposited.

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12
Q

How is a waterfall formed?

A

1) A layer of softer rock such clay is covered partly by a harder more resistant rock such as granite.
2) Hydraulic action erodes the uncovered weaker rock and creates a plunge pool that begins to undertrack towards the weaker rock underneath the harder rock.
3) The overhanging harder rock collapses
4) The collapsed rock causes more erosion through ablation.
5) therefore a large drop structure is formed called a waterfall

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13
Q

Waterfall formation key words?

A
  • Resistant rock
  • Less resistant rock
  • Plunge Pool
  • Undercutting
  • Overhang
  • Hydraulic action
  • Abrasion
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14
Q

What is a gorge?

A

The retreating path of a waterfall and is a narrow cleft with steep rocky walls, normally with a stream flowing through it.

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15
Q

How is a gorge formed by erosion?

A

Same as a waterfall, however this process of weaker rock eroding and leaving the more resistant rock to overhang and eventually collapse is repeated. Additionally, vertical erosion takes part in this process.

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16
Q

Name the five ways in which a gorge can be formed.

A

-Erosion
-Geological uplift
-Erosion and geological uplift
-Melting of glaciers
-backwards pathway of waterfalls

17
Q

What is Lateral erosion?

A

It is the eroding of the banks (sides) of a river, broadening it.

18
Q

What is vertical erosion?

A

the eroding of the bed of a river, deepening it.

19
Q

Example of a uk Gorge?

A

Cheddar Gorge.

20
Q

How was cheddar gorge in england formed and what shape is it?

A

By periglacial flooding, and the shape near scarps loop where it exits into a valley, the cross section is far more wide than earlier on in the coarse.

21
Q

What are interlocking spurs?

A

Interlocking spurs are the winding shape of a river around higher land made from more resistant rock.

22
Q

How are interlocking spurs formed?

A

The river winds around the harder rock and instead erodes the softer rock by ts side, creating s shaped structure.

23
Q

What is a v-shaped valley?

A

An elongated depression between uplands hills or mountains, formed by erosion and weathering or the melting of glaciers.

24
Q

How is a v-shaped valley formed?

A

Vertical erosion causes the river bed descend and the depression between the upland to elongate. Weathering causes the soil/rock on the step like sides of the valley to loosen and be washed into the river/ slope transport.

25
Q

What is weathering?

A

Weathering is the deterioration of rocks, soils and minerals through contact with water, atmospheric gases, sunlight and biological organisms.

26
Q

How are Meanders and and ox-bow lake formed?

A

1)The water’s discharge will bend around the harder rock, hitting an area of softer rock and therefore erode it. This causes a bend.
2) By hydraulic action, the rapid water hits and erodes the inner curve of the bend, and sedimentation will occur on the outer curve, causing the curve to almost create a full circle.
3)Due to throughway, once the neck is cut and the circle comes together, the water will flow in a straight line and not around the meander.
4) sedimentation cuts of the meander, and an oxbow lake is formed.

27
Q

Meander key words

A

-Throughway
-sedimentation/deposition
-erosion

28
Q

What is a Slip off slope and how does it form a meander?

A

The water moves around the raised area of sand and shingles, the slip off slope, and undercuts the bank causing the bend.

29
Q

What is a floodplain and where are the found?

A

Expansive flat land (with silt build up) either side of a river that floods when the river has too much discharge.
Lower coarse.

30
Q

How do levees form in a floodplain?

A

When there is too much discharge, the water will overflow onto the floodplain. As the water travels over the rover banks, it loses energy and immediately deposits its larger sediment. This builds up to form wall like structures called levees which in turn, raises the river channel and decreases its chance to flood again.

31
Q

What occurs in the upper course of a river?

A

Lots of vertical erosion and therefore v-shaped valleys, waterfalls, and interlocking spurs.

32
Q

What occurs in the middle course of a river?

A

More lateral erosion, causing more formations such as meanders.

33
Q

What occurs in the lower course of a river?

A

Same as the middle coarse, however with more room for discharge, there is less pressure and energy causing deposition and formation of islands.

34
Q

Why do rivers flood? x3

A
  • Saturated or too dry soil.
  • Paving over soil, creating an impermeable surface
    -Deforestation (plants absorb water)
35
Q

What is a hydrograph?

A

The rate of flow/ discharge versus the time past, showing how a river is affected by a storm/ lots of rainfall.

36
Q

Hydrograph analysis

A
  1. Lag time- the time between the peak rainfall and peak discharge
  2. Peak discharge
  3. Peak rainfall- on the bar chart
  4. Raising limb
  5. Falling limb
  6. Baseflow/ antecedent- normal flow of the river.
  7. Bankfull discharge- horizontal line showing when a flood might occur
37
Q

What causes the lag time?

A

The water from the peak rainfall will be absorbed in the soil or by plants, causing it to become throughflow (flowing underground), preventing it from reaching the river quickly.

38
Q

What affects the length of the lag time?

A

If the soil is saturated, or too dry or has an impermeable surface such as pavement covering it (urban areas) water will not be absorbed and therefore will become runoff and join the river quickly, causing more discharge.

39
Q

What are the four stages in a hydrograph?

A

1) Channel precipitation- during the lag time, water falling directly on a rivers surface within a channel.
2) Overflow- during the rising limb, water begins to raise over the banks of a river.
3) throughflow- during the falling limb, runoff has ceased and the water flows much slower into the river through the soil
4) Groundwater flow- During the baseflow and end of the falling limb, it is the very slow movement of water through porous rocks into the river.