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Earth's Layers – Crust, Mantle, Core

Delhi Police & SSC Exams Preparation

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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)

1

The outermost layer of the Earth is called?

Options: (A) Mantle (B) Crust (C) Core (D) Asthenosphere

Category: Basic Layers

Show Answer

B. Crust

2

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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