NDA Geography · Earth's Structure, Landforms and Geological Time
Earth's Interior, Crust and Plate Tectonics
The Earth is built in shells — crust, mantle, core — separated by discontinuities, and its rigid outer shell is broken into plates whose movements build mountains, open oceans and ring the Pacific with fire.
Why this matters
15 PYQs and the densest-HARD subtopic in the chapter. Two ideas earn most of the marks: the layer order and what each layer is made of (inner core SOLID, outer core LIQUID), and the three plate-boundary types. Get the lithosphere definition and the major-vs-minor plate list cold.
Concept 1 of 6
The layers of the Earth and the lithosphere
Intuition
Definition
The shells, outside in:
- Crust — the thin outermost skin (oceanic 5–10 km, continental 30–70 km).
- Mantle — silicate rock down to ~2900 km. Its upper part includes the asthenosphere, a partially-molten, slowly-flowing layer that the plates ride on.
- Outer core — LIQUID iron-nickel; its motion generates Earth's magnetic field.
- Inner core — SOLID iron-nickel (solid despite being hottest, because the pressure is enormous).
Lithosphere = crust + uppermost SOLID mantle (the rigid plate layer). It sits ON TOP of the soft asthenosphere. The lithosphere is thickest under the great mountain belts (deep crustal roots) and thinnest under the oceans.
Worked example
- The crust is the outermost skin you stand on.
- Below it lies the mantle, the thick silicate shell.
- Below the mantle is the liquid outer core.
- At the centre is the solid inner core.
Practice this conceptself-check · 3 quick reps
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Practice — Level 1 (3 reps)
Quick reps to lock in the method. Try each, then check.
- 1.Which is solid — the inner core or the outer core?
- 2.Lithosphere = crust + ?
- 3.Where is the lithosphere thickest?
From the bank · past-year question
[Q131 · Sep · 2019]
Lithosphere is NOT just the crust
Hottest is not always liquid
Concept 2 of 6
Discontinuities between the layers
Intuition
Definition
The named boundaries, surface inward:
- Conrad — within the continental crust (upper 'sial' over lower 'sima').
- Mohorovicic (Moho) — separates the crust from the mantle.
- Repetti — within the mantle (upper / lower mantle).
- Gutenberg — separates the mantle from the outer core.
- Lehmann — separates the outer core from the inner core (the innermost discontinuity).
| Discontinuity | Separates | Position |
|---|---|---|
| Conrad | Upper / lower crust | Shallow |
| Mohorovicic (Moho) | Crust / mantle | Base of crust NDA 2022 — Moho is THE crust-mantle boundary. |
| Repetti | Upper / lower mantle | Mid-mantle |
| Gutenberg | Mantle / outer core | Deep |
| Lehmann | Outer core / inner core | Innermost NDA 2023 — Lehmann is the deepest, in the innermost part of the Earth. |
Practice this conceptself-check · 3 quick reps
Try it yourself
Practice — Level 1 (3 reps)
Quick reps to lock in the method. Try each, then check.
- 1.Which discontinuity separates the crust from the mantle?
- 2.Which discontinuity lies between the mantle and outer core?
- 3.Name the innermost discontinuity.
From the bank · past-year question
[Q92 · Sep · 2022]
Moho vs Gutenberg
Concept 3 of 6
Oceanic vs continental crust
Intuition
Definition
Key contrasts:
- Oceanic crust — thin (~5–10 km), DENSE, basaltic ('sima', rich in silica + magnesium). Being heavier, it subducts beneath continental crust.
- Continental crust — thick (~30–70 km), LIGHT, granitic ('sial', rich in silica + aluminium).
- The crust is brittle, not plastic — it fractures, which is why plate edges and faults exist.
- Most of the Earth's internal heat is stored in the mantle; convection in the MANTLE (not the crust) drives the plates.
Worked example
- Compare densities: oceanic crust is basaltic and dense; continental crust is granitic and light.
- The denser slab cannot ride over the lighter one — it sinks.
- So the oceanic slab subducts beneath the continental slab.
Practice this conceptself-check · 3 quick reps
Try it yourself
Practice — Level 1 (3 reps)
Quick reps to lock in the method. Try each, then check.
- 1.Which crust is denser, oceanic or continental?
- 2.Continental crust is rich in which two elements (sial)?
- 3.Where is most of the Earth's internal heat stored?
From the bank · past-year question
[Q129 · Sep · 2022]
Convection is in the MANTLE, not the crust
Oceanic crust is thinner, not thicker
Concept 4 of 6
What the crust is made of
Intuition
Definition
- The continental crust is mostly silicate minerals — feldspar (~half the crust) and quartz are the most abundant; pyroxene, amphibole and mica are the common dark (ferromagnesian) minerals.
- A rough crustal-abundance order among the dark minerals tested by the NDA: mica < amphibole < pyroxene.
- Crust also stores groundwater in its pore spaces. Whether rainfall becomes groundwater depends on precipitation amount, evaporation rate, and the ground's ability to let water infiltrate — not on how far the site is from the sea.
Worked example
- Mica is comparatively minor among the three.
- Amphibole is somewhat more abundant.
- Pyroxene is the most abundant of the three.
Practice this conceptself-check · 3 quick reps
Try it yourself
Practice — Level 1 (3 reps)
Quick reps to lock in the method. Try each, then check.
- 1.Which mineral makes up about half the Earth's crust?
- 2.Order by crustal abundance: mica, amphibole, pyroxene.
- 3.Name one factor that does NOT control groundwater recharge.
From the bank · past-year question
[Q87 · Apr · 2025]
Concept 5 of 6
Tectonic plates and their boundaries
Intuition
Definition
Major plates (7): Pacific, North American, South American, Eurasian, African, Indo-Australian, Antarctic. Minor plates include Cocos, Nazca, Caroline, Philippine, Arabian, Juan de Fuca. The three boundary types:
- Convergent (collide): oceanic-continental → SUBDUCTION + volcanic arc + deep trench (Andes); continental-continental → fold mountains (Himalayas); oceanic-oceanic → island arcs (Japan).
- Divergent (separate): mid-ocean ridges, sea-floor spreading, new land (Mid-Atlantic Ridge — Iceland sits on it, giving geothermal energy, new land and tourism).
- Transform (slide past): strike-slip faults (San Andreas).
The Ring of Fire circles the Pacific — a belt of convergent subduction zones, hence an active seismic AND volcanic zone with deep trenches.
Worked example
- The Mid-Atlantic Ridge is where two plates pull apart — a divergent boundary.
- Rising magma there gives geothermal heat, builds new land, and draws tourists.
Practice this conceptself-check · 4 quick reps
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Practice — Level 1 (4 reps)
Quick reps to lock in the method. Try each, then check.
- 1.Name the boundary type that builds the Himalayas.
- 2.What forms at a divergent boundary in an ocean?
- 3.The San Andreas Fault is which boundary type?
- 4.Is the Antarctic Plate major or minor?
From the bank · past-year question
[Q109 · Apr · 2018]
Antarctic is a MAJOR plate
Ring of Fire ≠ purely convergent
Concept 6 of 6
Folds and crustal deformation
Intuition
Definition
Fold types by how far compression has tilted the axial plane:
- Symmetrical / upright — axial plane vertical.
- Asymmetrical — axial plane inclined.
- Overturned — one limb pushed past vertical.
- Recumbent — axial plane virtually HORIZONTAL (extreme compression, the fold lies on its side).
- Isoclinal — both limbs parallel (dipping the same way).
Folding at convergent boundaries is how fold mountains (Himalayas, Alps) are raised.
Worked example
- Upright = vertical axial plane; asymmetrical/overturned = inclined.
- As compression lays the fold flat, the axial plane approaches horizontal.
- That extreme is the recumbent fold.
Practice this concept2 quick reps
Practice — Level 1 (2 reps)
Quick reps to lock in the method. Try each, then check.
- 1.A fold whose axial plane is horizontal is called?
- 2.Folding builds which class of mountains?
From the bank · past-year question
[Q115 · Sep · 2019]
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)
Discontinuities between the layers5 rows
| Discontinuity | Separates | Position |
|---|---|---|
| Conrad | Upper / lower crust | Shallow |
| Mohorovicic (Moho) | Crust / mantle | Base of crust NDA 2022 — Moho is THE crust-mantle boundary. |
| Repetti | Upper / lower mantle | Mid-mantle |
| Gutenberg | Mantle / outer core | Deep |
| Lehmann | Outer core / inner core | Innermost NDA 2023 — Lehmann is the deepest, in the innermost part of the Earth. |
Watch out for (7)
- Lithosphere is NOT just the crust→ The layers of the Earth and the lithosphere
- Hottest is not always liquid→ The layers of the Earth and the lithosphere
- Moho vs Gutenberg→ Discontinuities between the layers
- Convection is in the MANTLE, not the crust→ Oceanic vs continental crust
- Oceanic crust is thinner, not thicker→ Oceanic vs continental crust
- Antarctic is a MAJOR plate→ Tectonic plates and their boundaries
- Ring of Fire ≠ purely convergent→ Tectonic plates and their boundaries
Mastery check — 5 interleaved questions
Try each one before clicking. Questions are interleaved across the concepts above, not grouped — interleaving sharpens transfer.
[Q66 · Sep · 2021]
[Q133 · Apr · 2023]
[Q104 · Apr · 2026]
[Q55 · Sep · 2021]
[Q115 · Apr · 2024]
Drill every past-year question on this subtopic
15 questions from the bank — paginated, with cart and Word-export support.