Structure of the Interior of the Earth

The Earth is composed of three main layers: Crust, Mantle, and Core. Each layer differs in composition, thickness, and physical state.

1. Crust

The outermost layer of the Earth.

It is the thinnest layer (about 570 km).

Two types:

Continental Crust thicker, mainly made of granite.

Oceanic Crust thinner, mainly made of basalt.

It is solid and forms the surface where we live.

2. Mantle

Located below the crust, extends up to about 2900 km.

It is the thickest layer of the Earth.

Divided into:

Upper Mantle

Includes Lithosphere (rigid) and Asthenosphere (semi-molten).

The asthenosphere allows plate movement.

Lower Mantle (Mesosphere)

Mostly solid due to high pressure.

Contains magma chambers and is responsible for volcanic activity.

3. Core

The innermost layer, extending from 2900 km to 6371 km.

Composed mainly of iron and nickel (Ni + Fe).

Divided into:

Outer Core

Liquid state

Causes Earths magnetic field.

Inner Core

Solid state

Due to extremely high press

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