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Faulting of the Earth’s Crust                           The  Himalayan  region  is  one  of  the  most  sensitive
            Faulting occurs in rocks when they are subjected to     regions in the world prone to earthquakes since it is
            stress that is stronger than the internal strength of the   located between two continental plates: the Indian
            rock. This causes it to fracture, thus causing a fault.   and the Eurasian plates. The Indian plate continually
            When blocks of rocks get dislocated from a plane, a     pushes  northward  a  few  centimetres  each  year,
            fault or a deep crack occurs.                           shoving its way under the Tibetan plateau.
            Faulting  can  occur  in  any  direction  with  the  blocks   Regions in India prone to earthquakes are Kashmir, the
            moving  away  from  each  other  in  both  vertical  and   Western  and  Central  Himalayas,  North  and  Middle
            horizontal directions.                                  Bihar, the North-East Indian region, the Rann of Kutch
                                                                    and the Andaman and Nicobar group of islands.
            Earthquakes
                                                                    Measuring Earthquakes
            This sudden shaking of the Earth's crust is called an
                                                                    Earthquakes  spread  energy  in  the  form  of  seismic
            earthquake.
                                                                    waves which are measured by a seismograph which
                                                                    produces  a  digital  graphic  recording  of  the  ground
                                                                    motion  caused  by  the  seismic  waves.  The  digital
                                                                    recording is called a seismogram.
                                                                    The Richter scale measures the strength or intensity of
                                                                    the shock waves produced by an earthquake. Richter
                                                                    scale  magnitudes  are  based  on  a  logarithmic  scale
                                                                    with base 10. An increase of one numeral on the scale
                                                                    would  represent  ten  times  the  magnitude  on  the
                           Occurrence of earthquake
                                                                    seismograph chart.
            Earthquakes  are  most  common  in  regions  that  are
            prone to faulting. Faults occur where two plates meet.              Wow Fact
            Earthquakes usually originate deep inside the Earth's
                                                                                On  25  April,  2015,  a  magnitude  7.8
            crust, where the pressure between two plates is so                  earthquake inflicted severe damage to the
            great that they cannot be held in place. Due to the                 nation of Nepal, causing several Himalayan
            release of pressure, the rocks inside the crust snap,               mountains  to  shrink,  including  Mount
            sending  shock  waves  or  seismic  waves  out  in  all             Everest which shrunk by one inch.
            directions.  The  point  inside  the  Earth  where  the
            earthquake originates is called the focus. The point on   Volcanoes
            the surface that is vertically above the focus is called
                                                                    A volcano is an opening or a vent in the Earth’s crust
            the epicentre.
                                                                    through which molten magma, ash and gases come
                                                                    out from below the surface. Volcanoes are generally
                                                                    found where tectonic plates converge or diverge. The
                                                                    best  example  of  convergent  tectonic  plates  is  the
                                                                    Pacific  Ring  of  Fire  and  that  of  divergent  tectonic
                                                                    plates is the Mid-Atlantic Ridge. Volcanoes can also
                                                                    form in places where the Earth's crust is subjected to
                                                                    stretching  and  thinning,  such  as  in  the  African  Rift
                                                                    Valley.
                                                                    Hotspots are usually located where the heat of the
                                                                    Earth's  mantle  creates  a  column  of  hot,  molten
                                                                    material  to  rise  until  it  reaches  the  crust.  The
                                                                    temperature melts the rocks in the crust forming pipes
                      Focus and epicentre of an earthquake
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