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Rivers SEC ONE TEXTBOOK PAGE 101
38

Sec 2 rivers 2013

Sep 03, 2014

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Page 2: Sec 2 rivers 2013

What is a river?

• A river is a natural watercourse, usually freshwater, flowing towards the sea.

• Without the hydrological cycle, rivers cannot be formed.

Page 3: Sec 2 rivers 2013

HYDROLOGICal CYCLE

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HYDROLOGICAL

CYCLE

SURFACE RUNOFF

INFILTRATION

CONDENSATION

TRANSPIRATION AND EVAPORATION

PRECIPITATION

Page 5: Sec 2 rivers 2013

HYDROLOGICAL CYCLE

• Precipitation – water from clouds come to the Earth’s surface as rain, snow and hail• Transpiration – plants release water vapour into atmosphere

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HYDROLOGICAL CYCLE

•Surface Run-off – rain that falls on Earth’s surface flows over land

• Condensation – water vapour rises, cools and changes into tiny water droplets

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HYDROLOGICal CYCLE

• Infiltration – water that soaks into the soil subsurface

• Percolation – water moves further down into the underlying soil after infiltration

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HYDROLOGICal CYCLE

•Throughflow – infiltrated water that flows sideways in the soil subsurface

• Interception – water is absorbed by trees

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RIVER SYSTEM

• Source – the starting point of a river• Mouth – the ending point of a river• Drainage Basin – The area drained by a river and its tributaries

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RIVER SYSTEM

•Confluence – the point at which a tributary joins the main river • Watershed – The boundary formed by the edges of the drainage basin

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Waterfalls

• Sudden, steep and vertical flow of fast-flowing water falling from great heights

• Formed by river erosion

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Niagara Falls on Niagara River, Canada and USA

• formed by erosion of rock of different resistance

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Formation of Waterfalls

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Formation of Waterfalls• River flows across rocks of different

resistance.

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Formation of Waterfalls

• River erodes the less resistant rock more rapidly• This cause a change in the gradient of the river

course.

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Formation of waterfalls• Over time, river plunges from a great height to

hit the riverbed below, • This forms a waterfall.

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Formation of plunge pools

• Repeated pounding of the river bed leads to a depression at the base of a waterfall

• A plunge pool is formed.

Page 20: Sec 2 rivers 2013

Meander

Note: Outer Bank = Concave Bank

Note: Inner Bank = Concave Bank

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Floodplain

Levees

FloodplainAreas of low-lying ground adjacent to a

river at the lower course

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Formation of Floodplain and Levee

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Formation of Floodplain and Levee

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Floodplain and Levee• During a heavy rainfall, river water

overflows its bank. River loses speed as it encounters friction.

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Floodplain and Levee• Deposition occurs as river’s energy decreases. • Coarser and heavier sediments are deposited

nearer to the river bank. • Finer and lighter sediments are deposited

further away.

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Formation of Floodplain and Levee

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Floodplain and Levee• Overtime, the accumulation of fine

sediments results in the formation of flat plains

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• Coarser and heavier sediments are acculumated

• Results in the formation of raised banks • Known as levees.

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Formation of Delta• At the river mouth, a river loses energy and starts to deposit its sediments.

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DistributariesDelta

Over time, the accumulated sediments that rise over the water and the distributaries form a delta.