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    Physical features of India

    Physical

    features of

    India

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    India y

    featuresThe 6 physical features are :The Himalayan mountains

    The northern plains

    The peninsular plateau

    The Indian desertThe coastal plains

    The Islands

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    Indian Deserts

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    The Himalayas

    The Himalayas are geologically young andstructurally fold mountains which stretchover the northern borders of India .These mountain ranges run in a west east

    direction from Indus to rahmaputra.Himalayas covers a distance of about!"##$m . Their width varies from "##$m in%ashmir to &'#$m in (runachal Pradesh .

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    Longitudinal divisionThe Himalaya consist of three parallel ranges in its

    longitudinal e)tent :The northern most rangeis $nown as the inner

    Himalayas or the Himadri . It is most continuous rangeconsisting of the loftiest pea$s with an average height of

    6###m . It consist of all prominent Himalayan pea$s .The range lying to the south of Himadry forms the most

    rugged mountain system and is also $nown as Himachalor lesser Himalaya . The altitude varies between *+##

    and "'##m and the average width is of '# $m . Thisrange is famous for hill station li$e %angra and %ulluvalley .

    The outer most range of the Himalayas is called the,hiwali$s . They e)tend over a width of -'#$m andhave an altitude varying between ## m . This

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    divisionThe Himalaya has been divided on the basis of

    regions from west to east . The part of Himalayalying between Indus and satlu0 has beentraditionally $nown as Pun0ab Himalayas . Thepart of Himalayas lying between satlu0 and $ali

    rivers is $nown as $umoun Himalayas . The $aliand the tista rivers demarcate the 1epalHimalayas . (nd the Himalayas lying betweentista and dihang rivers is $nown as (ssam

    Himalayas . The Himalayas which spread alongthe eastern boarders of India is $nown aspurvachal .

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    1orthern plains

    The northern plain has been formed by the

    interplay of three ma0or river systems 2 the Indus 3the rahmaputra 3the 4anga along with theirtributaries . This plain is formed of alluvial soil . Thedeposition of alluvium in a vast basin lying at the

    foothills of the Himalaya over millions of years 3formed this fertile plain . It spreads over an area of+ la$h s5.$m . The plain being about !"##$m longand !"# to*!# $m broad 3 is a densely populatedphysiographic division . /ith a rich soil covercombined with ade5uate water supply andfavorable climate it is agriculturally a veryproductive part of India .

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    The peninsular plateau

    The peninsular plateau is a table landcomposed of the old crystalline ,igneous and metamorphic rocks . Itwas formed due to the breaking and

    drifting of gondwana land and thusmaking it a part of the oldestlandmass . This plateau consist of 2

    broad divisions :the entralhighlands and the !eccan plateau .

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    entral "ighlands#nd !eccan Plateau

    The part of the peninsular plateau lyingto the north of 1armada river covering ama0or area of alwa plateau is $nown as

    7entral highlands .The Deccan plateau is a triangularlandmass lying to the south of river

    1armada . The ,atpura range 8an$s itsbroad base in the north while theahadev 3 the %aimul hills and the ai$alrange form its eastern e)tension .

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    /estern 4hats/estern 4hats lie parallel to the western coast

    . They are continues and can be crossedthrough passes only . The western 4hats arehigher than the eastern 4hats . Their averageelevation is ## to &6## m . The western

    4hats cause orographic rain by facing the rainbearing moist winds to rise along the westernslopes of then 4hats . The western 4hats are$nown by di9erent local names . The highest

    pea$s include anai mudi and the doda betta

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    4hats$astern %hats are lower than&estern %hats. The averageelevation of $astern %hats is '((mts. The $astern %hats stretchfrom the )ahanadi *alley to the+igiris in the south. The $astern

    %hats are discontinuous andirregular and dissected by riverdraining into the ay of engal.

    )ahindragiri is the highest peak

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    The Indian deserts

    The Indian Deserts lies towards the western

    margins of the (ravali hills . It is an undulatingsandy plain covered with sandunes this regionresives very low rainfall below &'# mm per year .It has arid climate with low vegetation cover .

    ,treams apear during the rainy season . ,oonafter they disappear into the sand as they do nothave enough water to reach the sea . ;uni is theonly large river in this region . archans coverlarger areas but longitudinal dunes become moreprominent near the indo Pa$istan boundary .

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    The coastal plainsThe peninsular plateau is 8an$ed by stretch of narrow

    coastal strips 3 running along the (rabian sea on thewest and the bay of engal on the east . The westerncoast 3 sandwiched between the western 4hats and the(rabian sea is a narrow plain . It consist of three

    sections . The northern part of the coast is called the$on$an 3 the central stretch is called the $annad plainwhile southern is referred to as the alabar coast theplains along the bay of engal are wide and level in the

    northern part 3 it is referred to as the northern circar 3while the southern part is $nown as $oramandal coast .;arge rivers such as the ahanadi 3 the 4odavari 3 the%rishna and the $avery have former e)tensive delta onthis coast . ;a$e chili$a is an important feature along

    the eastern coast

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    The islandsesides a vast main land 3 India has also !

    groups of islands . The ;a$shadweepislands close to the alabar coast of %eralais composed of small coral islands . It

    covers small area of *! s5 . %m and$avarathi island is the administrative head5uarters . This island group has greatdiversity of 8ora and fauna the pity island 3which is uninhabited3 has a bird sanctuary .

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    (ndaman and 1icobar

    The (ndaman and nicobar islands islocated in the bay of engal they arebigger in si

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    )#!$ 0 :

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