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What physical processes shape our landscapes?

The geomorphic processes that shape landscapes: weathering (mechanical, chemical and biological) and mass movement; and the processes of erosion, transport and deposition by rivers and the sea.

A focused answer to OCR GCSE Geography B (J384) Distinctive Landscapes on the geomorphic processes that shape landscapes, covering mechanical, chemical and biological weathering, mass movement, and erosion, transport and deposition.

Generated by Claude Opus 4.810 min answer

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  1. What this dot point is asking
  2. Weathering
  3. Mass movement
  4. Erosion, transport and deposition
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What this dot point is asking

This is OCR GCSE Geography B (J384) Component 1, Our Natural World, within Distinctive Landscapes: "What physical processes shape our landscapes?" OCR expects you to explain the geomorphic processes that wear down and reshape the land: weathering (mechanical, chemical and biological) and mass movement on slopes, and the processes of erosion, transport and deposition carried out by rivers and the sea. These processes are the toolkit you then apply to coastal and river landforms.

Weathering

Weathering matters because it produces the loose material that gravity, water and the sea then move and shape. The dominant type depends on climate and rock: freeze-thaw is common in cold uplands, carbonation on limestone in wetter areas.

Mass movement

On a coast, mass movement helps a cliff retreat: once waves undercut the base, the unsupported rock above slumps or falls.

Erosion, transport and deposition

These three processes move material and build landforms. They are carried out by both rivers and the sea, often with the same named processes.

Erosion wears material away:

  • Hydraulic action: the sheer force of moving water (and, at the coast, air compressed into cracks by waves) breaks rock apart.
  • Abrasion: rocks and sand carried by the water scrape and grind against the bed, banks or cliff, wearing it away like sandpaper.
  • Attrition: transported rocks knock against each other, becoming smaller and rounder over time.
  • Solution (corrosion): weak acids in the water dissolve soluble rock such as limestone and chalk.

Transport moves the eroded load:

  • Traction: large boulders rolled along the bed.
  • Saltation: smaller pebbles bounced along.
  • Suspension: fine sand and silt carried within the water, making it look cloudy.
  • Solution: dissolved minerals carried in the water.

Deposition drops the load where the water loses energy: in a river's lower course where the gradient eases, on the inside of meanders, in sheltered coastal bays, or where a river enters the sea or a lake.

Try this

Q1. Describe the difference between weathering and erosion. [2 marks]

  • Cue. Weathering breaks rock in place; erosion wears it away and carries it off.

Q2. Explain how transport moves material of different sizes in a river. [4 marks]

  • Cue. Traction rolls boulders, saltation bounces pebbles, suspension carries fine sand and silt, and solution carries dissolved minerals.

Exam-style practice questions

Practice questions written in the style of OCR exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.

OCR 20194 marksExplain how mechanical and chemical weathering break down rock. (Component 1)
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A 4-mark "Explain" question assessing AO1 and AO2 of weathering processes. Markers reward a developed mechanism for each type.

Award credit for: mechanical (physical) weathering breaks rock without changing its chemistry, for example freeze-thaw, where water enters a crack, freezes and expands by about 9 percent, widening the crack until fragments break off. Chemical weathering changes the minerals in the rock, for example carbonation, where rainwater is a weak carbonic acid that slowly dissolves limestone and chalk. Top answers explain the mechanism (water freezing and expanding; acid dissolving rock), not just name the types.

OCR 20216 marksExplain how the processes of erosion, transport and deposition work together to shape a river or coastal landscape. (Component 1)
Show worked answer →

A 6-mark "Explain" question marked by levels of response, assessing AO1 and AO2 of linked processes.

Strong answers explain erosion wearing material away (hydraulic action, abrasion, attrition, solution), transport moving it (traction, saltation, suspension and solution carry the load downstream or along the coast), and deposition dropping it where energy falls (in slow water, sheltered bays, or as a river enters the sea). They then link the three: a river erodes its bed and banks in the upper course, transports the load as the gradient eases, and deposits it in the lower course to build floodplains and deltas; a coast erodes headlands, transports sediment by longshore drift, and deposits it as beaches and spits. A good answer shows the sequence rather than defining the three in isolation. Markers reward the linked chain.

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