Geography - 9230 OxfordAQA

Section C: Physical Landscapes - Coastal Landscapes

Akopọ

Stand on a cliff top and nothing appears to be happening. Waves arrive, waves go back, and the rock looks permanent. It is not. A wave breaking against a cliff can generate pressures of tens of tonnes per square metre, and it does so several thousand times a day, every day, for centuries. The coastline you are standing on is a snapshot of a process that has not stopped and will not.

This lesson gives you the machinery to read any coast in an exam photograph. You will learn what makes a wave constructive or destructive, the four families of process that shape a shoreline, and how rock type and geological structure decide which landform appears where. You will build headlands, bays, caves, arches, stacks, beaches, spits and bars from those processes rather than memorising them as pictures. Then you will weigh the engineering that people use to hold the line, and follow one enormous scheme in the region from the reasons it was built to the conflicts it caused.

Awọn Afojusun

  1. The Middle and Far East have a range of diverse landscapes.
  2. The coast is shaped by a number of physical processes.
  3. Distinctive coastal landforms are the result of rock type, structure and physical processes.
  4. Different management strategies can be used to protect coastlines from the effects of physical processes.
  5. An overview of the location of major upland/lowland areas and river systems.
  6. Wave types and characteristics. Coastal processes:
  7. weathering processes - mechanical, chemical
  8. mass movement - sliding, slumping and rock falls
  9. erosion - hydraulic power, abrasion and attrition
  10. transportation - longshore drift
  11. deposition - why sediment is deposited in coastal areas.
  12. How geological structure and rock type influence coastal forms.
  13. Characteristics and formation of landforms resulting from erosion - headlands and bays, cliffs and wave cut platforms, caves, arches and stacks. Characteristics and formation of landforms resulting from deposition - beaches, sand dunes, spits and bars. Examples should be used from the region and integrated into the teaching of the content. The costs and benefits of the following management strategies:
  14. hard engineering - sea walls, rock armour, gabions and groynes
  15. soft engineering - beach nourishment and re-profiling, dune regeneration, mangroves
  16. managed retreat - coastal realignment.
  17. An example of a coastal management scheme in the region to show:
  18. the reasons for management
  19. the management strategy/strategies
  20. the resulting effects and conflicts.

Àwòrán ọpọlọ

A ti ṣe àwòrán kókó yìí kí o lè rí bí àwọn èrò ṣe so pọ̀.

Ṣí àwòrán ọpọlọ nínú áàpù

Akọ̀wé Ẹ̀kọ́

Every stretch of coast is settling an argument between the energy arriving from the sea and the resistance of the material meeting it. Where the energy wins, the coast retreats and you get cliffs, caves, arches and stacks. Where the material wins, or where the energy is spent before it arrives, sediment settles and you get beaches, spits and bars. Nothing on a coastline is decorative. Each landform is the visible answer to that one calculation, and once you can run the calculation yourself you can explain a photograph you have never seen before.

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Oriire fun ipari ẹkọ lori Section C: Physical Landscapes - Coastal Landscapes. Ni bayi ti o ti ṣawari naa awọn imọran bọtini ati awọn imọran, o to akoko lati fi imọ rẹ si idanwo. Ẹka yii nfunni ni ọpọlọpọ awọn adaṣe awọn ibeere ti a ṣe lati fun oye rẹ lokun ati ṣe iranlọwọ fun ọ lati ṣe iwọn oye ohun elo naa.

Iwọ yoo pade adalu awọn iru ibeere, pẹlu awọn ibeere olumulo pupọ, awọn ibeere idahun kukuru, ati awọn ibeere iwe kikọ. Gbogbo ibeere kọọkan ni a ṣe pẹlu iṣaro lati ṣe ayẹwo awọn ẹya oriṣiriṣi ti imọ rẹ ati awọn ogbon ironu pataki.

Lo ise abala yii gege bi anfaani lati mu oye re lori koko-ọrọ naa lagbara ati lati ṣe idanimọ eyikeyi agbegbe ti o le nilo afikun ikẹkọ. Maṣe jẹ ki awọn italaya eyikeyi ti o ba pade da ọ lójú; dipo, wo wọn gẹgẹ bi awọn anfaani fun idagbasoke ati ilọsiwaju.

  1. Which process wears down sediment itself rather than the coastline? A. Hydraulic power B. Abrasion C. Attrition D. Solution Answer: C
  2. Which type of mass movement leaves stepped, back tilted terraces in a soft clay cliff? A. Rock fall B. Sliding C. Slumping D. Soil creep Answer: C
  3. Headlands and bays are most likely to form along which type of coast? A. A concordant coast B. A discordant coast C. A coast made of a single uniform rock D. A coast with no exposed rock Answer: B
  4. Which of the following is soft engineering? A. Rock armour B. Gabions C. Beach nourishment D. A curved sea wall Answer: C
  5. What is the main disadvantage of building groynes? A. They reflect wave energy and scour the beach in front of them B. They starve the coast downdrift of sediment C. Their wire cages corrode within a few decades D. They can only be built on tropical coasts Answer: B

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