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    Mountains in Europe

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    1) Alaska range

    2) Southern Alps

    3) Dinaric Alps

    4) Atlas mountains

    5) Pyrenees

    6) aucasus

    !) Apennines") #aurus

    $) El%ur& an' (agros

    $) in'ukush

    1*) +irthar range

    11) +unlun Shan12) ,rals mountains

    13) Appalachian

    mountains14) -reat Di.i'ing/ange

    0ist o mountains to locate

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    • un'erstan'ing o the origin an'e.olution o earths crust

    • At the time o the ormation o theearth crust rst %asaltic crust o ocean %reaking an' melting a lightercontinental crust 'e.elope'

    • colli'e 7ith one another 8 a largerlan' mass

    •  #he 9oints 8 ol'mountains

    :mportance o mountain %uil'ing

    process

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    ,rals Mountains

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     #ypes o mountains

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    ;lock mountains ormation

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    Phases o Di.ergent continentalcrust

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    Arican rit .alley > %lock mountains

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    EuropeIndia

    E?ample o %lock mountains

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    Fold mountains

    •  #rue mountains

    • ompressi.e orce ol'ing

    • Due to collision oplates @ )

    • lookslike mountains

    Block mountains

    comparison

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    0an'orms on earth

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    Meaning

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    • /aise' lan' 'uring mountains%uil'ing process

    • Deposition rom la.a

    • Deposition rom 7in'

    • Ero'e' 'ue to glaciers

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    Intermontane plateau

    • ;oli.ia plateau

    • #i%etan plateau

    • olum%ia plateau

    • olora'o plateau

    • Anatolia Plateau@#urkey)

    • Deccan plateau

    • +atanga plateau• &ark plateau@,SA)

    • Ethiopianhighlan'

    Continental plateau

     #ypes o plateau

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    Glacial

    plateau

    • -rah7al

    plateau

    • 0aurentian

    plateau@ana'a)

    • olum%ia

    snakeplateau

    @,SA)• Deccan

    Plateau• Shanplateau

    Lava

    plateau

     #ypes o Plateau

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    Bolivia plateauColumbia- colorado

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    Ozark plateauAnatolia plateau

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    Loess plateauLaurentian plateau

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    • rigin o /i.erongo an'(am%e&i

    Dense euatorialorest

    • +no7n orresources

    -ol' 'iamon'sopper

    +atanga Plateau

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    • Euatorial region

    • Dense rainorest

    • +no7n or gol'reser.e

    Plateau o Mato -rasso ;ra&il

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    • Plateau crosse' %ySal7een ri.er

    • :rra7a''y ri.erpasse' in eastern

    si'e• Shan plateau chie

    source o lea' &incan' sil.er

    Myanmar• +no7n or teak

    orest

    @;urmese #eak)

    Shan plateau Myanmar

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    F/oo o the7orl'G > highest

    an' largestplateau

    • Source o:n'us

    ;rahmaputraSal7eenMekong

     Hangtse7ang e

    • :mp role in:n'ian

    monsoon

     #i%etan plateau

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    • -ranite

    • 0ess mo%ilecannot

    mo.eup7ar'

    • ;ack%one ool'

    mountains

    ;atholith

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    0an'orms on earth

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    Plains

    • Meaning

    • allu.ial plains ori.ers

    • Depositional plains

    /i.ers

    Sea @su%merge'coast)

    • Erosional plains Erosion o plateau

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    Asia Eur

    ope

    Afri

    ca

    Sout

    America

    !ort

    America

    :n'us Danu

    %e

    Bile Ama&

    on

    Mississippi >

    Missouri-anga >;rahmaputra

    /hine ongo

    ParanaParag

    uay

    olora'o

     Hangt&e@hina)

    /hone

    Biger St 0a7rence

    7ang e

    @hina)

    Po (am

    %e&i

     Hukon

    :mportant ri.er %asins o the 7orl'

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     Hangt&e ri.er hina

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    •  Hangt&e > 3th longest ri.er in the 7orl'

    • Ba.iga%le ri.er > 35I o hinas population

    • Sichuan %asin > rice culti.ation

    Shanghai > %iggest port o hina•  Juhan > :ron an' steel

    • Ban9ing > te?tile iron an' steel

    • heng'u > oil an' gas

    •  #hree gorge 'am

    •  Hun ho canal > connect Hangt&e 7ith 7ange

    :mportant locations

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    Euphrates #igris ri.er :ra

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    • 0ake Kan

    • 0ake ,rmia

    :mportant centers in :ra• ;agh'a' Mosul +irkuk Al ;asra

    0ocations near Euphrates#igris

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    Ama&on ri.er ;ra&il

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    • 0argest 2n' longest ri.er

    • Sel.as > euatorial rain orest

     #in ru%%er in Sel.as• Sertao > ranching region

    • Petroleum reser.e at the mouth

    Manaus > :ron ore na.iga%le•  plateau o Mato -rasso > gol'

    reser.e

    0ocations near Ama&on ri.er

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    Mississippi ,SA

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    •  #emperate grasslan's > Prairies

    • Jheat corn an' cotton culti.ation

    • :mportant cites

    • +ansas > agriculture

    • St Pitts%urg > iron an' steel

    Be7 rleans > port ship %uil'ing 

    0ocations near Mississippi %asin

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    MurrayDarling %asin Australia

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    •  #emperate grasslan' > 'o7ns

    • Jheat culti.ation

    • Sheep rearing Animal hus%an'ry

    • Jool an' 'airy pro'uction

     

    0ocation near Murray'arling %asin

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    0an'orms on earth

    Mountains @ol' an'%lock)

    Plateaus

    Plains

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    Batural atastrophic

    e.ents

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    .olcanism

    -eomor

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    complete seuence oprocesses o creation

    an' mo.ement omagma L creation o

    .olcanic lan'ormsKolcanism is notran'om

    /eason associate'7ith .olcanism is also

    not ran'om

    Kolcanism

    -eomorpho

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    1st

    • Pacic /ing o

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    O-O " #olcanic arc

    O-C "#olcanic

    mountains

    Plate mo.ements

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    2n' 

    • 'i.ergence

    • ;asaltic >peaceuleruption

    Mi' ceanic /i'ge

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    3th 

    • ;reaking up oMe'iterraneanplates intomultiple %locks

    • An'esiticeruption

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    Me'iterranean seais resi'ual part o #ethys sea

    •  #ethys sea 7as

    locate' %et7een >0aurasia an'-on'7ana

    • ollision o Arica to

    0aurasia > %reakingup o plates oMe'iterranean sea

    istory o Me'iterranean sea

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    • 4th 

    • Magma :slan' arc

    • Direction oplate

    • a7aii /eunion+urile Aleutian

    ot Spot Kolcanoes

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    Aleutian :slan's

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    Basaltic eruption

    • ccur at mi'oceanicri'ge an' hot spot.olcanism

    • ;asalt highly ui' >mo%ile

    • Sprea' across easily

    • Nuite eruption

    • Kolcanic arcs .olcanicmountains

    • An'esite > less ui' >less mo%ile

    • Soli'ies at short'istance intense

    pressure 'e.elopinsi'e >e?plosi.e

    Andesitic eruption

    comparison

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    Basaltic eruption Andesitic eruption

    comparison

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    Kolcanic 0an'orms

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    :ntrusi.e 0an'orms

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    :ntrusi.e 0an'orms

    •:ntrusion o Magma in se'imentary rocks

    •Sills @ori&ontal)

    •Dyke @Kertical)

    •0accolith > magma 7hich coul' not come out

    •0opolith > saucershape'

    •Phacolith > shape like 7a.es•;atholith > intrusi.e granitic rock

     

    :ntrusi.e Kolcanic 0an'orms

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    E?trusi.e .olcanic 0an'orms

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    ot spot .olcanoon continentalcrust

    • racks on

    continental crust >;asaltic eruption

    • Sprea' across the

    lan'• 0ayer o.er layer

    • EO Deccan la.atrapps

    0a.a plateaus

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    • :n'ian plate passe'o.er a hot spotnear /eunion

    :slan'• ;asaltic eruption

    • 0ayer o.er layers >looks like steps 8=

    Deccan la.a traps• Soil > %lack soil

    regur

    :n'ian Deccan trap

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    Spatial 'istri%ution o 0a.a Plateau

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    • olum%iasnakeplateau ,SA

    • &ark plateau ,SA

    ParanaPatagonia SAmerica

    • A'ama7a plateauArica

    • ;ie plateau Arica• +atanga Plateau

    Arica

    Deccan plateau :n'ia

    • Ara%ian plateau

    • ;alkan plateauEurope

    • Si%erian plateau/ussia

    •  Hunan Plateau hina

    • Shan plateauMyanmar

    • +im%erly plateauAustralia

    0ist o la.a plateaus o the 7orl'

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    E?trusi.e .olcanic 0an'orms

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    • Kolcanic :slan's@ot spot)

    • ighly ui' la.a

    @%asaltic) %uil''ome

    • -entle slope

    •Nuite .olcano

    • Kolcanoes oa7aii

    Shiel' Q Dome .olcano

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    • collision >

    .olcanicmountains

    • 0ess ui' la.a@An'esitic)e?plo'e .iolently

    • Kiscous la.asoli'ies at short

    'istance

    • Mt Paricutin Me?ico

    in'er cones

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    Kolcanic

    mountainsEach ne7eruption > ne7layers o ash orla.a

    Mt Strom%oli Mt

    Kesu.ius Mt

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    Sield$

    dome

    Cinder Composit

    eighlyui'

    0ess ui' Qhighly

    .iscous

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    • -eysers

    8ountains oot 7ater

    • -roun' 7aterheate' %y

    shallo7source omagma

    • l' aithulgeyser Hello7stone park,SA

    -eysers

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    • ot Spring

    • Jater reach'eep enough >heate' %yinterior

    • 0ocate any parto the 7orl'

    ot Spring

    - -Q h t 'DiCerence %et7een geyser an'

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    • -eyser > -Q7 heate'%y shallo7 magmasource

    • ot spring > gQ7heate' %y eithermagma source or

    heate' rocks• -eyser > cham%er in

    interior > pressure >comes out like

    ountain

    • ot >spring uite

    DiCerence %et7een geyser an'

    otspring

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    %e&ser

    • -eysers are rare

    ot 7ater 'issol.e'7ith silicaaccumulate' onsurace > gi.es'iCerent colours

    • ,SA Hello7stonepark

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    • eate' 7ateris taken out >use' ormo.ing

    tur%ine >generation oelectricity

    • oole' 7ater

    o7n %ackinto interior

    -eothermal energy

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    • DiRcult to locate a goo' source ogeothermal reser.oir 7ith currenttechnology

    • DiRcult to 'ig a 'eep 7ell 7ith har'an' hot %e'rock

    • armul gases can escape rom the

    earth interior 7hile e?ploration > --gases an' 'issol.e' to?ic elements

    0imitations o geothermal energy

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    .olcanism

    Su''en mo.ement or

    -eomor

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    Su''en mo.ement or.i%ration in earths

    crust

    /elease o the energy'ue to intense pressureL acti.e internal

    'ynamism o the earth

    Earthuake

    pho

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    1) Shallo7 ocus

    EN2) :nterme'iateocus EN

    3) Deep ocusEN

    Shallo7 ocus >

    'estructi.e

     #ypes o Earthuake

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    At (unction of ) plates

    Subduction of *aci+cplate

    Earthuakes in apan

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    1st 

    ollision oPlate%oun'aries

    collision

    collision

    collision

    /easons %ehin' EN

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    2n'

    Di.ergentPlate%oun'aries

    'i.ergenceM/

    /easons %ehin' EN

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    • 3th•  #rans.erse plate

    %oun'aries

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    4th 

    Me'iterraneansea region

    Bumerous smallplates

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    5th 

    raton 8 sta%le parto crust

    /eemergence o ol'ractures

    6th 

    uman :n'uce'

    1) /:S

    2) mining

    3) Buclear testing

    /easons %ehin' EN

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    .olcanism

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    i

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    !ormal ,aves

    Spee' > 1** kmph

    o.er shorter 'istances

    Ja.elength T1** km

    •Spee' > !** kmph

    • o.er longer 'istances

    • Ja.elength > = 15*km

    sunami ,aves

    comparison

    l th

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    • Distance %et7eent7o crests otroughs 8

    7a.elength

    • Ja.es o #sunami

    are 7i'er thannormal 7a.es othe ocean 7ater

    7a.elength

    Ph 1

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    • EN on ocean crust >uplit the 7aterup7ar'

    •  #sunami 7a.e

    generate'• Kessels in the mi'

    sea cannotrecongnise the

    tsunami 7a.es• Sea 7ater rece'e at

    the shore

    Phase 1

    Ph 2

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    • At coast > 'epth

    'ecrease >7a.elength'ecreases > 7a.eheight increases

    • A huge 7all o7ater > 1*12oor high create'

    Enormous energyrelease' at theshore

    Phase 2

    Ph 3

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    • it the coast

     #sunami not asingle 7a.e %utmultiple 7a.es

    • 4th an' "th 7a.es

    are the most'angerous

    •  #ime lapse

    %et7een each7a.es > 15 to 5*minutes

    Phase 3

    Ph t i

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    Phases o tsunami

    :n'ian prepare'ness against

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    •  #sunami Early 7arning system gi.es 7arning in1* minutes o su%marine earthuake

    • :n'ian Bational centre or cean :normationSciences @:B:S)y'era%a'

    •  #o capture #sunami 7a.e amplitu'e on 24?!%asis

    •  real time seale.el sensors 7ith %ottom pressurerecor'ers

    • < ra'ars or coastal currents• oastal ti'e gauge stations

    :n'ian prepare'ness against

     #sunami

    atastrophic e.ents on

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    pearth

     #heir reasons an''istri%utions

    KolcanismEN

     #sunami