Earth's Layers – Crust, Mantle, Core
Delhi Police & SSC Exams Preparation
1. Introduction
The Earth is made up of several layers arranged like an onion. Each layer has unique composition, density, and temperature. Studying these layers helps us understand earthquakes, volcanoes, and the Earth's magnetic field.
Key Study Areas:
- Layer composition and characteristics
- Depth ranges and temperatures
- Geological significance
- Exam-focused memory tricks
Practical Importance:
Understanding Earth's structure helps explain natural phenomena and geological processes
2. Major Layers of the Earth
The internal structure of the Earth is divided into three main layers:
| Layer | Depth (approx.) | Composition | Key Facts |
|---|---|---|---|
| Crust | 0–35 km | Silica (Si) & Aluminium (Al) — "SIAL" | Outermost solid layer |
| Mantle | 35–2900 km | Silica (Si) & Magnesium (Mg) — "SIMA" | Semi-molten rock called magma |
| Core | 2900–6371 km | Nickel (Ni) & Iron (Fe) — "NIFE" | Hottest and densest layer |
3. The Crust — The Skin of the Earth
Characteristics:
- Thinnest layer of the Earth
- Average temperature: ~500°C
- Two types: Continental and Oceanic
Continental Crust
Thick (avg 35 km), granitic composition
Oceanic Crust
Thin (avg 5 km), basaltic composition
Composition Memory Aid:
"SIAL" = Si + Al → found in continents
"SIMA" = Si + Mg → found below oceans
4. The Mantle — The Middle Layer
Key Features:
- Occupies most of Earth's volume (about 84%)
- Made of semi-molten rock (magma)
- Average temperature: ~1000–3000°C
Mantle Divisions:
Upper Mantle (Asthenosphere)
Semi-molten, causes plate movement
Lower Mantle (Mesosphere)
Solid due to high pressure
5. The Core — The Center of the Earth
Core Characteristics:
- Temperature: >5000°C
- Composition: Nickel + Iron (NIFE)
- Extreme pressure conditions
Outer Core
Molten iron and nickel → causes Earth's magnetic field
Inner Core
Solid due to extreme pressure
Memory Tricks:
"C-M-C" = Crust–Mantle–Core
"SIAL–SIMA–NIFE" = Elements order
Earth's Internal Layers Diagram
CRUST (SIAL) - 0–35 km
MANTLE (SIMA) - 35–2900 km
OUTER CORE (Molten NIFE) - 2900–5150 km
INNER CORE (Solid NIFE) - 5150–6371 km
6. Quick Comparison Table
| Feature | Crust | Mantle | Core |
|---|---|---|---|
| Depth | 0–35 km | 35–2900 km | 2900–6371 km |
| Composition | Si, Al | Si, Mg | Ni, Fe |
| State | Solid | Semi-solid | Outer – liquid, Inner – solid |
| Temperature | ~500°C | 1000–3000°C | >5000°C |
| Importance | Surface layer, supports life | Plate movement | Magnetic field |
PYQs (Previous Year Questions – Delhi Police & SSC)
The outermost layer of the Earth is called?
Options: (A) Mantle (B) Crust (C) Core (D) Asthenosphere
Category: Basic Layers
Show Answer
B. Crust
Which layer of the Earth is made up of Si and Al elements?
Options: (A) Crust (B) Mantle (C) Core (D) Lithosphere
Category: Composition
Show Answer
A. Crust
Questions 3-7 continue with the same format. Complete all questions for comprehensive practice.
Final Exam Tips
Remember "SIAL–SIMA–NIFE" formula
Outer Core → Liquid → Magnetic Field
Inner Core → Solid due to high pressure
Asthenosphere = upper mantle → plate movement zone
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