Denudation
ICSE Class 9 · Geography · Chapter 10
What this chapter covers
- Meaning and agents of denudation
- Work of river
- Stages of a river course
- Landforms associated with a river course
- Work of wind
Key definitions
Hydraulic action is the wearing away of the banks and bed by the sheer force of moving water, which pushes into cracks, compresses the air inside and loosens pieces of rock.
Abrasion is the wearing away of the bed and banks by the sand, pebbles and boulders that the river hurls and rolls against them, much as sandpaper wears away wood.
Attrition is the wearing down of the load itself as the pebbles and boulders knock against one another and against the bed.
Solution is the dissolving of soluble rock minerals, especially limestone, in the slightly acidic river water.
Deflation is the lifting and blowing away of loose, dry, fine particles of sand and dust from the ground by the wind.
Key points
- Denudation is the wearing down and lowering of the land by weathering, mass movement and erosion, with the removal of the loosened material; it is the work of exogenic forces.
- The agents of denudation are running water, wind, glaciers, sea waves and underground water; each erodes, transports and deposits.
- The work of an agent depends mainly on its speed and volume: fast, full agents erode, slow ones deposit.
- A river erodes by hydraulic action, abrasion, attrition and solution, and transports its load by traction, saltation, suspension and solution.
- Vertical erosion deepens a valley; lateral erosion widens it.
- The upper course (youthful stage) is steep and fast and does vertical erosion; the middle course (mature stage) does lateral erosion and transportation; the lower course (old stage) is almost level and deposits.
- A V-shaped valley forms in the upper course where the river cuts down faster than the sides are worn back; a very deep and narrow one is a gorge.
- A waterfall forms where a river crosses hard rock over soft rock or the edge of a plateau; undercutting and collapse make it retreat upstream and leave a gorge.
- A meander is a loop-like bend with a steep river cliff on the outer bank and a gentle slip-off slope on the inner bank; a cut-off meander becomes an ox-bow lake.
- A delta is triangular land built of fine sediment at a river's mouth in a shallow, calm sea; the Ganga-Brahmaputra delta is the world's largest, while the Narmada and the Tapi form estuaries.
- Wind is the chief agent in deserts, where rain and plants are scarce and loose sand is plentiful; it erodes by deflation, abrasion and attrition.
- A deflation hollow is a depression scooped out by wind and stops deepening at coarse pebbles or moist ground; an oasis may form where water reaches the surface.
- A sand dune has a gentle windward slope and a steep leeward slope and moves downwind; barchans are crescent-shaped with horns pointing downwind, and seifs are long ridges parallel to the wind.
Questions answered
Define denudation. Name the three processes it includes.
Distinguish between weathering and erosion.
Name five agents of denudation. Which is the most important on land, and which is dominant in deserts?
Explain any three ways in which a river erodes its bed and banks.
Name the four ways in which a river transports its load.
State two differences between the upper course and the lower course of a river.
Explain how a V-shaped valley is formed. Why does it form in the upper course?
Describe the formation of a waterfall where a band of hard rock lies over soft rock. Why does the waterfall retreat upstream?
Past board exam questions
ICSE 2019 sample paper · 3 marks
Give a geographical reason for each of the following: (i) Volcanic activity and earthquakes occur in the same belt. (ii) All rivers do not form a delta. (iii) Chemical weathering is more common in the tropical regions.
Show answer
ICSE 2019 sample paper · 3 marks
Explain the meaning of the following terms: (i) Deflation hollow (ii) River meander (iii) Block disintegration.