Structure of the Earth (Foundation)

STRUCTURE OF THE EARTH 

CORE IDEA

Earth has a layered internal structure with different composition and physical properties → explains earthquakes, volcanoes, plate tectonics

1. COMPOSITIONAL LAYERS

Layer

Depth

Composition

Keyword

Crust

0–35 km

Silica + Alumina

SIAL

Mantle

35–2900 km

Silica + Magnesium

SIMA

Core

2900–6371 km

Nickel + Iron

NIFE

2. CRUST

  • Outermost, supports life
  • Continental (thick, less dense)
  • Oceanic (thin, more dense)

👉 Key: Continental ≠ Oceanic

3. MANTLE

  • Largest layer (~84%)
  • Semi-solid, plastic

👉 Drives plate movement

4. CORE

  • Outer core → liquid
  • Inner core → solid

👉 Generates magnetic field

5. PHYSICAL LAYERS (IMPORTANT)

Layer

Nature

Lithosphere

Rigid

Asthenosphere

Plastic

Mesosphere

Solid

Core

Liquid + solid

6. SEISMIC EVIDENCE

Wave

Property

P-wave

Solid + liquid

S-wave

Only solid

👉 S-wave absence → liquid outer core

7. UPSC TRAPS

  • Lithosphere = crust + upper mantle
  • Asthenosphere ≠ liquid (plastic)
  • Oceanic crust more dense
  • Inner core solid despite heat
  • Core = NIFE

8. 5-SECOND REVISION

👉 SIAL → SIMA → NIFE
👉 Crust → Mantle → Core

MAINS LINE

“Earth’s layered structure, inferred mainly from seismic waves, explains its internal dynamics and surface processes.”

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