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(ov) Continental Drift Thesyy propoundid by Alfred fos ltrjoq Alfred Weannrschange th perspective ( , ¥ othin actentinat anc not doing dre that Hr Witmer a3) hy thoy one yak taney y Va r iy funouy, So, too he gave hy pos Wien — Chant ever ahiplol DM fevered Proent minnel moatenrtal fanaa < Oo forrned —> beoat ges oe Be be of sh ebol =) bbe ally tec indian xeoons (Anganabnd) Lawnony'a Tethys seo Cond Wana 7 TT OID LL | h 4 as Paley dh proes She petentiat atudy r ¢) Toreeniwe — Attn one Mn phate, art pha Ces dhurr gtoqy abhrc ih abs be tore pi }uation ann Pome> 5 ald ® folio climatic evidint® — Ratie me a g Enis CUE (® Corals 2 off Ihe cook of Canada rR TIN AAa 2 Aan aah > Penineutox 1% @M rlactal evidences —<_ Hao pitee Suawal'a ® Coal 1 Grado # Glan Wie } Hee forer+ buried undir sedi nth and clus to high pressune der ppXotuXe broman convert Into feat dat Lyj nite =n Brjuminows —5 mos+> (Creal sty Paar: Arun Anthvackte Chhota Nagpo vegton Ly Sek ed Rnown 08 Coobing» cook le r Coal dormathon > Den ge Kesen} rv Ne ee) \ % Canada % UGridatwe not have Nh ‘gh demp 1 % (Coal In formed in high dium perotwu Bek dhin tn ave garqrafrbrcal pridumtt, Fosat ls — vpnaining port of Living orqonior™ PHS logical & Vik eae a ae Seuth Prarie Fra SS 7 Cunognathus, ye70% i eset’? we onegn ‘ South Parca te ~y “4 Lyuphogorns — Meso poyoud Clamoabtenb = gbind sae Alas : = Means gonduona Aan el es Lava bao Toot | Mogntyse of = Align itaelf 1) mines SS Bene a the magnititn of tanth Re = Mag nhtned =~ Mn —S divechsn A ! ! 4 Tt shoos Anithn qj = Ges) y Pel Q Otlont'c Ocean mouth Sem per Year maa + All the tmp hold mins prount | a GiAiin, — Kalgoorlie —_— Cool gordic ne ———- os = Lo Ld > lool % poll j / Gl Cri hel Lym >) [Force © Accovcling to COT 2 Ca) Equatey word movemuntc —> Forte of Suyancy Uertwenol Moverrunt an dial fee > >~ Pole Fleeing = (t's y the Troy OHH Chri ok cor) (2) 2) WT. Wegequacy af} fore —r > @ @ 5) co 9 ( col, 2 @ae1ts OMe PN ety ete CCT, a Mentle conver ton oy « iving foy Ce Y pe Holmen BUg gented the} heot hom yaologettve dé : montle G reader earth's TMese ¢ ununty Carre Atay nat the Comnvetsion cunruntp - \ oa hos magma to rhe, spread 5 cook and AInk, Didhe» phar ¢ TeV OR a ae dhe | tr ¢cOT) driving the Ploter. spend of Hhl bce Coe etre diift— Url he + tipe explain , Che coulol nos Nebed tJeqenonr dhe force behind continuntal movement, 1b Holme, providad a plaus! ble mechaninm « Ye proposed Hot fonveetion cunt ta dhe Mantle pull the continents aponk or pr h Yorn together: : pn formaton of Oceanic ond — Holmer theowy explalnnd Beat loor ppreading , pubdu ction ONY ; Contrental featwre, mid oceanic Viel ay ond whe ned cwt fyma and old crust ty recycled back jnto the mantle. } Plo y Hanny hus 1960) oe Sea t loo Spreading theory a 4 - fl (® Formation BL ee Ce yt 072) the. SS Se mantle rly Hrroug h mi ocean aclg es ) cooln , and policifies ae form neu oceanic “Crush ges e® Movemunt of Otcan Pliner = imate tLe eminrger the newly formed crust pushes ane sida oceanic cruat tana from the 7 widge , Causing the ocean floor + > prend e G@ Subductim and vec yeltng — The oldin crust e verily athks — bacle Pato the mantle at Bubdiscton zane aan Dew Rigi) er a The pea-Flosy Spreading they 9 mechan) Lr. Weies. 6 dnb t ce that dectonre plots moves dur to we Convethon, Plate Tecientcs — Li thopphire = Cymtt upper Asthenonphure — Pant of mantle ort mantels plates ane ths beoben 529 which actually flo@ady over Plates ant conmrfantly uy motion —? dhey ae. going & tke do inten achons dhty pater ig known a8 plate tectonics The acholans have rebnt fea + mayor pdater thet ant prenect avin thy earth . These platey ar — © North Ameucon plate ® Soluth Ament can Plote. Pacific plate ® Ewmosian plate © Mha'com plobe © Trdo- Aurtrallan plate ao ride eamnans GB Anton eile plate OF One p, lat dhe « i torstintly in meting ae ae Bolin atin See Gen Hime period f Gk -) a n > nod ba si £ rte ¢ ~~ ei het t aa forth plete i ae Ca Ne (> inde mpi such ion nee —— a ae. ae One Ta peakeg Over aunphenosbhuu % doing Undeata chore - joes Interact ons t ay Cree : Divergun te Transfoon| plsuhp, part s- pPiwagence ae 2 types a cliven gence hare been obSenrfved (©Ceamic =o ceanfe) By el eh iaiN Life : eS fe fi ae fy, = The Ba Ip diven ‘ A. 9, becoune of Shes of Con Veep ery ¢ Ws jx tu ANDRES Prone Umi eeant ray 4 : nd Voloantn Magan by abyo ke Lom er =m earth. ARAANSARA ps bel "8s F de highot achive volcano fe ip (suntan atathe werla! — aura Ranger ; Bree One (Kits m » | setsmnicity Seypalitw. eect: fink ( Gs ea plate ane derkuc hive) 2 p) atey yt lf converge , the plate Bonnie ' tea Bubdlacting become of thtp uns wil be SR: HE d th 1 pleb pull mot ~~ after = hos ki An rae of plate % melting x | ah j W9t amount of AOI O preape ~ a pee the conti prtoll plate Vol tan) es teak TUM ANE form ed A Berm city tebows “ap as There moun taths ant nod are / ‘ plate Mary fr oun tasmy an Thro 4g pI > pore Ubtance Coant Beibmr city —» Ts se lmenchen the Linton ie Wasa ty adh) ea he a Oh one acdy Alife, of bubduction. Fualty Bate ~ Plate dectoni Convergent a Pes uchon Divergent -— Conntructin Trantor an Consennotive Heeante 2 Oicbanic Convergent ee a Kain of volcantC i eee gael anth ae oe ® Treche 2 (>) Earthquebe Vso ve @ Thunamt sector + =) Dpaving dhe dime ob Oeeanit — Oceanse - pl conve on Ce the * plate What vals “hgowle and dunsen will be subdued Jindaninenth the bs danser ‘plocte The zone es » subdued lh GU 08 aubduitcton sone , th ii » collid OS fenrolt aon ds When The) dumer J lake “ates ub that fn ian of ? Slab pull movement bine it finds very high ’) , i) demperohones’ dua he tuhich- theo ceantc Plat Meh, melting - When thar ib huge amount of Mo am wants te escape and J+ Abonti rinin a inte “the criisty and the tn bibmatton = volcanic! Eslond arth the Alewhon Inland anal. @® Him alayan +) farvanchel + Amdiain oh coher a CA ported fut having Pe fammnchel (volcan ace — Barren trland t Dorince¢ veltare Noncandor island Yes Preamon Nicobar e _Trnavene | Comenvative flte mMenpin nage vecks| @® Plate = con serrredl je @ Hin inbensity Corth ee i) quoke { 1 plichlog past cath -Ouring the dime fh dliduhs past ether y 5 fe of platen frarsform fausldy ot created - TN thate type oF plate, haun dart dhite of nu'fun tnotruchdn year ; dus treetion of any plot. heveven. fore daformatin of plotes tohey plore . Burin Arty type of plete movement veuy high In temity conthquoke occu whyeh rads to heavy Josh of Life ancl property « (© SAN ANDREAS Faulk -7 USA (G9 sinters! @ ANATOLTAN Foult v 
