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Waves generated due to the disturbance in a             STRUCTURE OF EARTH
            hypocenter  are called shock waves or seismic           Earth consists of four layers :
            waves.
                                                                    (a) Inner core
            Point on the earth surface i.e. vertically above
                                                                    (b) Outer core
            the hypocentre is called as epicentre.
                                                                    (c) Mantle
            Instrument  that  records  the  intensity  of
            seismic waves is called seismograph.                    (d) Crust
                                                                    Core of the earth is composed of nickel and
            Study of earthquakes is called seismology.
                                                                    iron. Inner core is solid while the outer core is





































                                                           Structure of earth


                                                                    liquid. Silicate rocks that are rich in iron and
                                                                    magnesium form the mantle. Mantle is viscous
                                                                    in  nature.  Crust  is  ferromagnetic  due  to
                                                                    ferromagnetic nature as silicates in them.

                                                                    Mantle and crust form up the earth's surface.
                                                                    In addition to the mantle and crust elements
                                                                    surface  also  consists  of  large  pieces  (12  in
                                                                    number) called tectonic plates.

                                                                    Tectonic  plates  keep  on  moving  over  the
                                                                    earth's mantle and they also slide upon one
                                                                    another as a result of which plate boundaries
                                                                    become  weaker.  Weaker  boundaries  of
                            Tectonic plates of earth
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