Page 122 - SST Class 07
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Outer Core                                             sediments,  which  are  eventually  buried  under

             The outer core is made of liquid iron and nickel       more  sediment  and  changed  by  heat  and  pres-
             and is between 3,500°C – 4,000°C. As the liquid        sure.
             metal  swirls  around,  it  induces  a  current  that   Some rocks are even formed from the remains of
             generates  the  earth’s  magnetic  field.  Heat  from   living things.
             the  core  powers  the  convection  currents  in  the   Types of Rocks
             mantle. It is 2,900 km thick.                          Different  types  of  rocks  are  formed  different
             Inner Core                                             ways.  Thus,  they  have  different  characteristics
             The  inner  core  is  the  hottest  part  of  the  earth   with regard to their composition, colour, size and
             reaching  temperatures  between  4,000°C  –            texture. On the basis of their mode of formation,
             4,700°C, which are as hot as the surface of the        there  are  three  major  types  of  rocks—igneous,
             sun.  It is made of solid iron and nickel that are     sedimentary and metamorphic.
             under  so  much  pressure  they  cannot  melt.  It  is   Igneous Rocks
             1,200  km  thick  and  heavy  radioactive  elements    Igneous rock may form with or without crystalli-
             within the core generate the intense heat as they
                                                                    sation.  Below  the  Igneous  rock,  there  is  one  of
             decay.
                                                                    the three main rock types. Igneous rock is formed
               MATERIALS OF THE EARTH’S CRUST                       through the cooling and solidification of magma

                       (ROCKS AND MINERALS)                         or  lava  on  the  surface  as  intrusive  (plutonic)
             The lithosphere is made up of rocks and miner-         rocks  or  on  the  surface  as  extrusive  (volcanic)
             als. Rocks are those materials which are obtained      rocks.
             from the earth’s crust. They include not only the
             hard  materials  such  as  granite  and  marble,  but
             also soft and loose materials such as chalk, clay,
             sand and salt.
             How the Rocks are Formed?
             Rocks are made up of substances called minerals.
             Any  naturally  occurring  solid  substance  with  a
             definite chemical composition is called a mineral.

             All  rocks  are  formed  in  the  earth’s  lithosphere,
             which includes the earth’s crust and the top part                        Igneous Rocks
             of its mantle, where partially molten rock called
                                                                    This magma can be derived from partial melts of
             magma flows very slowly under the crust.
                                                                    existing rocks in either a planet’s mantle or crust.
             Some rocks are formed when magma gets close            Typically, the melting is caused by one or more of
             to the surface and slowly cools.                       three  processes—  an  increase  in  temperature,  a
             Some of that red-hot magma breaks through the          decrease  in  pressure  and  a  change  in  composi-
             earth’s  crust  to  form  fiery  volcanoes,  releasing   tion.
             lava  to  cool  quickly  on  the  surface  or  even    Igneous rocks have following characteristics :
             underwater.
                                                                    g    These rocks are hard and compact.
             Other rocks form as a result of the weathering of
                                                                    g    These rocks do not occur in distinct beds or
             older  rocks  and  erosion,  creating  layers  of
                                                                         stratus.

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