GCSE Geography – Erosional river landforms – interlocking spurs
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Question 1 of 18
1. Question
Which of the following is NOT a distinctive river landform?
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Question 2 of 18
2. Question
What is the start of a river called?
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Question 3 of 18
3. Question
What is the end of a river called, where it meets the sea?
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Question 4 of 18
4. Question
In what course of a river do interlocking spurs occur?
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Question 5 of 18
5. Question
In what course of a river does a ox-bow lake occur?
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Question 6 of 18
6. Question
As the river nears the sea, in the lower course, what might deposition form before the river reaches the sea?
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Question 7 of 18
7. Question
What is an embankment or ridge called, that runs alongside a river to prevent flooding?
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Question 8 of 18
8. Question
What is the term used to describe projections of high land that alternate from either side of a valley and project into the valley floor?
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Question 9 of 18
9. Question
What sort of gradient will be found next to an interlocking spur?
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Question 10 of 18
10. Question
What is the shape of the surrounding slopes alongside interlocking spurs?
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Question 11 of 18
11. Question
What term describes fast-flowing turbulent sections of a river where the river bed has a relatively steep gradient?
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Question 12 of 18
12. Question
When a rivers gradient changes and/or the river bed becomes uneven, and the river’s flow becomes turbulent, what may occur within the rapids?
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Question 13 of 18
13. Question
Interlocking spurs occur because the water is not powerful enough to cut through the spurs and so has to flow around them. So where do spurs occur?
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Question 14 of 18
14. Question
What are interlocking spurs caused by?
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Question 15 of 18
15. Question
Where, along a river, are rapids found?
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Question 16 of 18
16. Question
On an ordnance survey map, what does it mean when the contour lines are close together?
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Question 17 of 18
17. Question
In the upper course of a river, the river’s water volume and discharge are low. So what method of river erosion is prevalent?
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Question 18 of 18
18. Question
In upland areas the geology is hard rock. Freeze-thaw weathering gradually broadens the river. What shape will the valley be in these upland areas?
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