Geography - 9230 OxfordAQA

Section D: Physical Landscapes - Hot Deserts Or

Akopọ

This is the one section of Paper 1 where you get a choice. Section D offers hot desert landscapes as one question and river landscapes as the other, and you answer whichever one you have been taught. Both are shaped by the same idea: a moving fluid picks material up, carries it, and puts it down again when it runs out of energy. In a desert the fluid is usually air. In a river valley it is water. Everything else follows from that.

This lesson teaches both options in full, so that whichever your school has chosen you have it here, and so that the shared machinery is obvious. You will learn the wind and water processes that carve a desert, and build yardangs, zeugen, dunes, badlands, wadis, alluvial fans and salt lakes from them. You will follow a river from its steep headwaters to its estuary, explaining interlocking spurs, waterfalls, gorges, meanders, ox-bow lakes, levees and flood plains as you go. Then you will read a storm hydrograph, weigh hard engineering against soft, and follow the largest river management scheme on Earth from the floods that caused it to the arguments it is still causing.

Awọn Afojusun

  1. Hot deserts are shaped by a number of physical processes.
  2. Distinctive landforms result from different physical processes in hot deserts.
  3. Development of hot desert environments creates opportunities and challenges.
  4. River landscapes The shape of river valleys changes as rivers flow downstream.
  5. Distinctive fluvial landforms result from different physical processes.
  6. Different management strategies can be used to protect river landscapes from the effects of flooding.
  7. Aeolian (wind) processes:
  8. erosion - abrasion and deflation
  9. transportation - surface creep, saltation and suspension
  10. deposition - why wind deposits sediment. Water processes:
  11. erosion - abrasion and hydraulic power
  12. transportation - traction, saltation and suspension
  13. deposition - why water deposits sediment.
  14. Characteristics and formation of landforms resulting from the effects of the wind - yardangs, zeugen and dunes.
  15. Characteristics and formation of landforms resulting from water-badlands, wadis, alluvial fans and salt lakes. Examples should be used from the region and integrated into the teaching of the content. Use example(s) in hot deserts to illustrate:
  16. development opportunities in hot desert environments: oil and mineral extraction, energy, farming, tourism
  17. challenges of developing hot desert environments: extreme temperatures, water supply, inaccessibility.
  18. The long profile and changing cross profile of a river and its valley.
  19. Fluvial processes:
  20. erosion - hydraulic action, abrasion, attrition, solution, vertical and lateral erosion
  21. transportation - traction, saltation, suspension and solution
  22. deposition - why rivers deposit sediment.
  23. Characteristics and formation of landforms resulting from erosion - interlocking spurs, waterfalls and gorges. Characteristics and formation of landforms resulting from erosion and deposition - meanders and ox-bow lakes. Characteristics and formation of landforms resulting from deposition - levées, flood plains and estuaries. Examples should be used from the region and integrated into the teaching of the content. How physical and human factors affect the flood risk - precipitation, geology, relief and land use.
  24. The use of hydrographs to show the relationship between precipitation and discharge. The costs and benefits of the following management strategies:
  25. hard engineering - dams and reservoirs, straightening, embankments, flood relief channels
  26. soft engineering - flood warnings and preparation, flood plain zoning, planting trees and river restoration. An example of a river flood management scheme in the region to show:
  27. why the scheme was required
  28. the management strategy/strategies
  29. the social, economic and environmental issues.

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

A desert dune and a river meander look nothing alike, and students revise them as if they were separate subjects. They are the same machine running on different fuel. In both cases a fluid flows, and while it has energy it erodes and transports; where it loses energy it deposits. Wind and water even use the same three transport processes with the same names, saltation and suspension in both, surface creep in the wind and traction in the water. Learn the machine once and you have learned both options in Section D.

Àkọsílẹ̀ Ẹ̀kọ́ Pípé wà lórí Ohun Èlò Green Bridge

Gba ohun èlò Green Bridge CBT sórí fóònù tàbí kọ̀mpútà rẹ fún gbogbo ilé ìkàwé IGCSE: ìwé ìdánwò àtijọ́, ìlànà ìdíwọ̀n, àwòrán èrò, káàdì ìkẹ́kọ̀ọ́ àti ẹ̀kọ́ ohùn.

Awọn akọsilẹ ẹkọ ni kikun pẹlu awọn aworan apejuwe
Oluranlọwọ ẹkọ ti AI ṣe agbara rẹ
Ìdánwò àdáṣe onítọ̀kọ̀ tí a ń ṣàyẹ̀wò lẹ́sẹ̀kẹsẹ̀ tí o bá parí
O wa lori Android, Windows, macOS, ati Linux Áàpù iOS ń bọ̀ láìpẹ́

Ìdánwò Ẹ̀kọ́

Oriire fun ipari ẹkọ lori Section D: Physical Landscapes - Hot Deserts Or. 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 removes loose fine material from a desert surface and leaves coarse stones behind? A. Abrasion B. Deflation C. Saltation D. Attrition Answer: B
  2. Which landform is a fan shaped deposit at the point where a desert valley opens onto a plain? A. Yardang B. Zeugen C. Alluvial fan D. Playa Answer: C
  3. Which type of erosion dominates in the upper course of a river? A. Lateral erosion B. Vertical erosion C. Coastal erosion D. No erosion occurs Answer: B
  4. What is lag time on a storm hydrograph? A. The time from the start of the rain to the peak discharge B. The time from peak rainfall to peak discharge C. The time the river stays above bankfull discharge D. The time taken for discharge to return to normal Answer: B
  5. Which of the following is soft engineering for flood management? A. Building an embankment B. Straightening a channel C. Flood plain zoning D. Constructing a flood relief channel Answer: C

Ṣiṣẹ́ lórí àwọn ìbéèrè wọ̀nyí nínú ohun èlò náà

Ṣiṣẹ́ lórí àwọn ìbéèrè wọ̀nyí nínú ohun èlò náà

Ṣe Adaṣe Awọn Ibeere Idanwo Adaṣe

Ṣe o fẹ ṣe adaṣe awọn ibeere idanwo adaṣe nipa Section D: Physical Landscapes - Hot Deserts Or? Ṣe igbasilẹ ohun elo Green Bridge CBT lati wọle si awọn ibeere idanwo adaṣe ati awọn ayẹwo adaṣe kikun fun koko-ọrọ yii.

Ṣe igbasilẹ ohun elo naa lori Google Playstore

Gbogbo ohun ti o nilo lati ṣe dara julọ ninu JAMB, WAEC ati NECO.

Green Bridge CBT Mobile App
Asiko ẹkọ AI ti ara ẹni Chat Assistant
Ìbéèrè ìdánwò IGCSE, JAMB, WAEC ati NECO tó ju 200,000 lọ
Fiwọn 1200 Awọn akọsilẹ Ẹkọ ju.
Atilẹyin Aisinipo - Kọ ẹkọ Nigbakugba, Nibi gbogbo
Tẹ̀dí Green Bridge
Àkójọpọ̀ Ìtàn Lítíréṣọ̀ & Ìbéèrè Tó Lè Dáyéé ṣẹ́lẹ̀
Tẹle iṣẹ ṣiṣe rẹ ati ilọsiwaju rẹ.
Àlàyé tí ó jinlẹ̀ fún ìmòye tó jinlẹ̀.