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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