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Geography

The Earth’s Crust, The Mantle, The Core and their Respective Characteristics

takriban dakika 6 kusoma

Mada za sehemu hiiStructure Of The EarthMada 3
  1. The Earth’s Crust, The Mantle, The Core and their Respective Characteristics
  2. Types of Rocks of the Earth’s Crust
  3. Simplified Geological Time Scale

The inner zones of the earth constitute the internal structure of the earth. The internal structure of the earth consists of three zones:

  1. Crust / Lithosphere
  2. Mantle / Mesosphere
  3. Core / Barysphere
Structure of the earth

Crust

  1. The outermost and thinnest zone of the earth, found between 8–50 km (or 5–30 miles).

  2. Also known as the Lithosphere.

  3. Largely composed of igneous rocks (crystalline, hard, and brittle).

  4. Consists of two layers:

    • Sial:
      • Outer layer of the crust.
      • Rich in silica and aluminum minerals.
      • Forms the basis of the continent.
    • Sima:
      • Found beneath the sial layer.
      • Separated from sial by the Conrad discontinuity line.
      • Composed of silica and magnesium.

Mantle

  1. Also known as the Mesosphere.

  2. Found between the crust and the core.

  3. Separated from the crust by the Mohorovic discontinuity (Moho).

  4. Extends downward to about 2900 km (1800 miles).

  5. Temperatures may reach about 5000°C.

  6. Consists of two parts:

    • Upper Mantle:
      • Rigid and together with the crust forms the lithosphere.
    • Lower Mantle:
      • Less rigid.
      • Forms the asthenosphere (molten layer within the Earth's interior).

Core

  1. The innermost zone of the Earth's structure.

  2. Also known as the Barysphere or Centrosphere.

  3. Diameter of about 6900 km (4300 miles).

  4. High density.

  5. Divided into two parts, separated from the mantle by the Gutenberg discontinuity:

    • Outer Core:
      • Liquid in nature due to high temperature (up to 3700°C).
      • Composed of nickel and iron (NIFE).
      • Thickness of about 2100 km.
      • Density of about 10.5 g/cm³.
    • Inner Core:
      • Solid due to extremely high pressure.
      • Composed mainly of iron.
      • Diameter of about 2600–2700 km (1600–1700 miles).

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