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The upper course of the river

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Presentation on theme: "The upper course of the river"— Presentation transcript:

1 The upper course of the river
What are the main processes that operate in the upper course? What landforms occur in the upper course of a river? How are the landforms created? Learning objectives

2 How does a river change from source to mouth?
Think, pair, share

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4 Many people think that rivers flow faster in upper course – why?
Lower course Upper course

5 Is it true though?

6 The Bradshaw Model Positive changes Negative changes
Explain to students – get them to note down on their long profile diagram the changes. Get verbal feedback after activity. Negative changes

7 The Bradshaw Model Activity:
Choose 3 characteristics to explain (including at least one positive and one negative)- use page 66 (tomorrow's geography ) to help Explain to students – get them to note down on their long profile diagram the changes. Get verbal feedback after activity.

8 How does the channel cross section change as you move from the source to the mouth?
Why does it change in this way?

9 Exam practice

10 Mark scheme

11 Exam practice

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13 Watch the video of the upper course of a river….
When complete you will be undertaking the following activities: Describe characteristics of the upper course of the river? What processes are happening? What landforms are found?

14 Landforms in the upper course
V-shaped valleys and interlocking spurs Rapids Waterfalls river disappears from view hidden by this spur of land River Conwy (near Mignant Moor)

15 Why do V-shaped valleys occur?

16 4 mark question…explain the formation of a V shape valley

17 Interlocking spurs In the upper course the river does not have a huge amount of energy to erode as it does not have a high discharge and it has to transport large pieces of sediment. When the river meets areas of harder rock that are difficult to erode it winds around them. A series of hills form on either side of the river called spurs. As the river flows around these hills they become interlocked. So, a series of interlocking spurs are often found in the upper course of a river valley.

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20 Techniques! – 1. Fieldsketching….
Produce an annotated fieldsketch to show that this is part of an upland river valley.

21 Waterfalls! Seljalandsfoss, SW Iceland

22 Waterfall formation

23 Waterfalls

24 How does a waterfall form?
Rearrange the stages of formation into the correct order:

25 Your labels should contain detailed explanations!
Waterfalls Draw and annotate a diagram to explain the formation of a waterfall. Suggested labels: More resistant rock Less resistant rock Plunge Pool Unsupported rock Fallen rocks Gorge Your labels should contain detailed explanations!

26 WATERFALL RETREATS . . UPSTREAM . . OVERHANG PLUNGE POOL UNDERCUTTING OF SOFT ROCK

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32 River load in upper course
Why are they rounded?

33 River load in upper course
Why are they rounded? Boulders are large and semi-rounded, due to attrition within the load and abrasion with the stream bed and banks

34 Skills (paper 1) linked to rivers


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