NDA Geography · Earth's Structure, Landforms and Geological Time
Weathering and Denudation
Weathering breaks rock down in place — physically by stress, chemically by reaction with water and air — and together with erosion and transport it wears the land down, a process called denudation.
Why this matters
10 PYQs and a GUARANTEED-MARKS pocket — 0% HARD over ten years. Almost every question is one of two kinds: sort a process as mechanical vs chemical, or spot the odd one out. Lock the two lists (mechanical processes; chemical processes) and the climate rule (chemical loves hot+humid, mechanical loves hot+dry), and this subtopic is free.
Concept 1 of 3: Weathering, erosion and denudation
Definition
- Weathering — in-place breakdown of rock (no transport).
- Mass wasting — downslope movement of rock/soil under gravity.
- Erosion — wearing away + removal by a moving agent (water, wind, ice).
- Denudation — the overall lowering of the land: weathering + mass wasting + erosion + transportation taken together. It is an exogenic (external) process.
Worked example
Practice this conceptself-check · 3 quick reps
The same idea in a real exam question:
Example 1 · Earth's Structure, Landforms and Geological Time · Weathering and Denudation
Concept 2 of 3: Mechanical (physical) weathering
Definition
Physical processes (no chemical change):
- Frost wedging — water freezes in cracks and expands.
- Salt-crystal growth — salts crystallise in pores and prise rock apart (a PHYSICAL process).
- Thermal expansion / exfoliation — repeated heating/cooling flakes off outer shells.
- Driving forces: gravity, expansion force, and water-pressure force.
- Mechanical weathering is most prevalent in hot dry deserts (and cold regions), where chemical reactions are slow. Granite hills weather into rounded tors.
Worked example
Practice this conceptself-check · 3 quick reps
The same idea in a real exam question:
Example 2 · Earth's Structure, Landforms and Geological Time · Weathering and Denudation
Salt-crystal growth is PHYSICAL
Concept 3 of 3: Chemical weathering
Definition
Chemical processes (mineral change):
- Solution — soluble minerals dissolve, leaching them away.
- Carbonation — carbonic acid attacks carbonates/feldspar.
- Hydration — minerals absorb water, swell and change (increases rock volume).
- Oxidation — oxygen reacts with iron, changing the rock's colour (reddening).
- Chemical weathering is strongest in a hot + humid climate.
- NOT chemical: thawing, exfoliation, frost action (these are physical).
| Process | What it does |
|---|---|
| Solution | Dissolves and leaches minerals |
| Carbonation | Acid attacks limestone / feldspar |
| Hydration | Minerals absorb water, swell, increase volume NDA 2021 — absorbing water and expanding is hydration. |
| Oxidation | Oxygen reddens iron-bearing rock |
Practice this conceptself-check · 3 quick reps
The same idea in a real exam question:
Example 3 · Earth's Structure, Landforms and Geological Time · Weathering and Denudation
Thawing and exfoliation are NOT chemical
Summary — formulas & gotchas at a glance
A revision cheat-sheet for the formulas and gotchas above. Click any concept name to jump back to its full explanation.
Reference tables (1)
Chemical weathering4 rows
| Process | What it does |
|---|---|
| Solution | Dissolves and leaches minerals |
| Carbonation | Acid attacks limestone / feldspar |
| Hydration | Minerals absorb water, swell, increase volume NDA 2021 — absorbing water and expanding is hydration. |
| Oxidation | Oxygen reddens iron-bearing rock |
Watch out for (2)
- Salt-crystal growth is PHYSICAL→ Mechanical (physical) weathering
- Thawing and exfoliation are NOT chemical→ Chemical weathering
Test yourself on Earth's Structure, Landforms and Geological Time
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