Inside Our Earth Summary Class 7 Geography Chapter 2

Planet Earth

• The earth in which humans live is not absolute spherical in shape.

Interior of earth

• The earth is like onion which is made up of several layers.

Crust

• The uppermost layer over the earth’s surface is called the crust.
• It is the thinnest of all the layers.
  • It is 35 km thick on the landmass (continental masses) and only 5 km on the ocean floors.
• Main mineral constituents of the continental mass: Silica and Alumina.
  • Thus, it is called sial (si-silica and al-alumina).
• The oceanic crust mainly consists of silica and magnesium
  • Thus, it is called sima (si-silica and ma-magnesium).

Mantle

• This layer extends up to a depth of 2900 km below the crust.

Core

• The innermost layer is the core.
• The radius of core is about 3500 km.
• It is mainly made up of nickel and iron.
  • Thus, it is called nife (ni – nickel and fe – ferrous i.e. iron).
• The central core has very high temperature and pressure.

Rocks

• Any natural mass of mineral matter that makes up the earth’s crust is called a rock.
• It can be of different colour, size and texture.
• There are three major types of rocks:
  • Igneous rocks
  • Sedimentary rocks
  • Metamorphic rocks

1. Igneous Rocks

• When the molten magma cools, it becomes solid and are called igneous rocks.
• They are also called primary rocks.
• There are two types of igneous rocks:
  • Intrusive rocks
  • Extrusive rocks

• When the molten lava comes on the earth’s surface, it rapidly cools down and becomes solid on the crust. These rocks are called extrusive igneous rocks.
  • They have a very fine-grained structure.
  • Example: Basalt. The Deccan plateau is made up of basalt rocks.
• When the molten magma cools down deep inside the earth’s crust giving formation of solid rocks are called intrusive igneous rocks.
  • Since they cool down slowly they form large grains.
  • Example: Granite. Grinding stones used to prepare paste/powder of spices and grains are made of granite.

2. Sedimentary Rocks

• Rocks roll down, crack, and hit each other and are broken down into small fragments which are called sediments.
• These sediments are transported and deposited by wind, water, etc. These loose sediments are compressed and hardened to form layers of rocks. These types of rocks are called sedimentary rocks. → Example: Sandstone is made from grains of sand.
• Sedimentary rocks may also contain fossils of plants, animals and other micro-organisms that once lived on them.

3. Metamorphic Rocks

• Under great heat and pressure, Igneous and sedimentary rocks can change into metamorphic rocks.
  • Example: clay changes into slate and limestone into marble.

Use of Rocks

• Rocks are used for construction activities such as making buildings, roads.
• They are source of minerals which are useful for various purposes in daily life.

Rock Cycle

• The process of transformation of the rock from one to another is known as the rock cycle.
• It describes the changes among the three main type of rock i.e., Igneous, Sedimentary and Metamorphic rocks.
  • When the molten magma cools; it solidifies to become igneous rock.
  • These igneous rocks are broken down into small particles by various agents such as weathering, temperature, wind etc. and are transported and deposited to form sedimentary rocks.
  • These smaller grains of rocks keep moving towards basins and lower regions and gradually form sedimentary rocks.
  • When the igneous and sedimentary rocks are subjected to heat and pressure they change into metamorphic rocks.
  • The metamorphic rocks which are still under great heat and pressure melt down to form molten magma.
  • This molten magma again can cool down and solidify into igneous rocks.

Note: These processes take hundreds and thousands of years.

Minerals

• Minerals are naturally occurring substances which have certain physical properties and definite chemical composition.
• These are very important for humans.
• For example, coal, natural gas and petroleum. They are also used in industries – iron, aluminium, gold, uranium, etc, in medicine, in fertilisers, etc.