NDA Geography · Earth's Structure, Landforms and Geological Time
Soils
Soil is the thin living layer that forms where weathered rock, climate, organisms, topography and time meet; soil-forming processes and a global classification organise its many types.
Why this matters
5 PYQs. The earners are the soil-forming FACTORS (parent material, climate, organisms, topography, time — never 'human habitation'), the named soil PROCESSES (calcification, laterisation, podsolisation, gleisation), and a couple of classification facts (Histosols = organic soil).
Concept 1 of 3: How soil forms — the five factors
Definition
The five soil-forming factors:
- Parent material — the underlying rock that weathers into mineral grains.
- Climate — temperature and rainfall drive weathering and leaching.
- Organisms — plants, microbes and animals add humus.
- Topography (relief) — slope controls drainage and erosion.
- Time — soil deepens and matures over long periods.
Human habitation is NOT a soil-forming factor. Soil develops in distinct layers called horizons (O, A, B, C).
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 · Soils
Concept 2 of 3: Soil-forming processes
Definition
- Translocation — fine particles washed DOWN by eluviation (removal from upper horizon) and deposited lower by illuviation.
- Calcification — where evapotranspiration exceeds precipitation (dry climate), lime/calcium accumulates near the surface.
- Podsolisation — in cool Taiga (coniferous) forests, acids bleach and leach the topsoil.
- Laterisation — in hot wet tropics, silica is leached, leaving iron/aluminium oxides (red laterite).
- Gleisation — waterlogged, poorly-drained soils.
Process classes: translocation, enrichment, removal, transformation.
| Process | Where / what |
|---|---|
| Translocation | Eluviation (down) + illuviation (deposit) NDA 2025 — translocation = eluviation + illuviation. |
| Calcification | Evapotranspiration > precipitation (dry); lime builds up NDA 2023 — dry climate, evaporation exceeds rainfall → calcification. |
| Podsolisation | Taiga (coniferous) forest NDA 2023 — podsolisation is predominant in the Taiga forest. |
| Laterisation | Hot wet tropics (red laterite) |
Practice this conceptself-check · 3 quick reps
The same idea in a real exam question:
Example 2 · Earth's Structure, Landforms and Geological Time · Soils
Concept 3 of 3: Soil classification (soil orders)
Definition
- Histosols — ORGANIC soils, rich in peat/decayed plant matter (waterlogged).
- Aridisols — dry desert soils.
- Oxisols — deeply weathered, iron/aluminium-rich tropical soils.
- Vertisols — clay-rich soils that swell and crack (like India's black cotton soil).
| Soil order | Character |
|---|---|
| Histosols | Organic (peaty) NDA 2023 — Histosols are the organic soil. |
| Aridisols | Dry desert soils |
| Oxisols | Weathered tropical soils |
| Vertisols | Swelling clays |
Practice this conceptself-check · 2 quick reps
The same idea in a real exam question:
Example 3 · Earth's Structure, Landforms and Geological Time · Soils
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 (2)
Soil-forming processes4 rows
| Process | Where / what |
|---|---|
| Translocation | Eluviation (down) + illuviation (deposit) NDA 2025 — translocation = eluviation + illuviation. |
| Calcification | Evapotranspiration > precipitation (dry); lime builds up NDA 2023 — dry climate, evaporation exceeds rainfall → calcification. |
| Podsolisation | Taiga (coniferous) forest NDA 2023 — podsolisation is predominant in the Taiga forest. |
| Laterisation | Hot wet tropics (red laterite) |
Soil classification (soil orders)4 rows
| Soil order | Character |
|---|---|
| Histosols | Organic (peaty) NDA 2023 — Histosols are the organic soil. |
| Aridisols | Dry desert soils |
| Oxisols | Weathered tropical soils |
| Vertisols | Swelling clays |
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