The Theory of Plate Tectonics Ppt

8/20/2019 The Theory of Plate Tectonics Ppt

1/37

THETHE

THEORY OFTHEORY OF

PLATE TECTONICSPLATE TECTONICS


2/37

CONTENTSCONTENTS

Introduction

Syllabus content

CLIL lesson

preparation


3/37

INTRODCTIONINTRODCTION

S!"ECT# General GeologyLE$EL: University (intermediate)

%ODL TITLE# Tectonic geology

NIT# The theory of plate tectonics

CLASS DRATION# 90 minTHE CLASS:

introduction (10 min)

main part (75 min)

the content tet: !5 minutes

activities: "0 min

closure (5 min)


4/37

SYLLA!S CONTENTSYLLA!S CONTENT

Focus only on #hat has $een covered in language classes upto the content class in %uestion&

Lan&ua&e ite's: simple'past present'continuous tense forms#ord order comparison of adectives articles use and plural

of nouns& *uture +imple Tenses structures #ould $e used as anintroduction to the tense topic itself in the language class&,ther language forms such as perfect tenses passivesconditionals are left out&

Clil class content unit# language forms of present'continuoustense forms future simple tense forms adective comparisonarticles use and plural of nouns&


5/37

CLIL LESSON PREPARATIONCLIL LESSON PREPARATION

CONTENT O!"ECTI$ES# +tudents #ill revise their prior -no#ledge a$out the theory of

continental drift and evidence that support that theory

students #ill learn a$out the theory of plate tectonics #hich

eplains the continental drift they.ll learn a$out plate $oundaries and their types and they.ll learn a$out #hat events

these movements can cause&

+tudents #ill also learn a$out the process of convection

currents #hich causes the plate movement&


6/37


LAN(A(E O!"ECTI$ES#

+tudents #ill revise voca$ulary from the previous class:

continental drift /angaea aurasia Gond#ana litosphere mantle

crust layers seafloor spreading reverse polarityNe) *ocabulary# rigid tectonic plates plate $oundary divergent

convergent transform collide denser' less dense smaller #armer

large largest midocean ridge slide su$duction trench

convection convection currents


7/37


Lan&ua&e structures# The /resent +imple'2ontinuous Tense

structures:

The theory of plate tectonics states&&&

The place #here t#o plates meet3

There are three types of3The plates are moving3

The *uture +imple Tense structures:

There #ill $e3(earth%ua-es volcanoes3)

The plates #ill move3 (to#ards east'#est)

2omparative structures: largelarger the largest small

smallerthe smallest larger than smaller than


8/37


STRATE(IES and ACTI$ITIES# 4 or using %ui6 sheets to revise and connect to prior

-no#ledge using pictures images videos and concepts maps

to help students #ith understanding and ac%uiring ne#

voca$ulary the concepts and processes related to tectonic plates and their movement using gapfilling activities

la$eling diagrams and ta$les to help students ac%uire ne#

voca$ulary and to practice language structures&

THIN+IN( S+ILLS# recalling identifying, recogni6ing comparing classifying

interpreting hypothesi6ing predicting producing eplaining


9/37

INTRODCTION PARTINTRODCTION PART


10/37


Continental dri-t .ui/ 0lin1in& to pre*ious 1no)led&e2rite the letter of the correct ans#er in the space provided&

888888 1& egener thought that all the continents #ere once together in on

large continent called

a& Gond#ana&

$& aurasia&

c& urasia&d& /angaea&

888888 & ;e# oceanic lithosphere forms as a result of

a& seafloor spreading&

$& normal polarity&

c& reverse polarity&

d& continental drift& 888888 !& vidence for seafloor spreading has come from

a& fossils in +outh


11/37


%atc3 t3e correct de-inition )it3 t3e correct ter'4 5rite

t3e letter in t3e space pro*ided4

88 "& hypothesis that states that the continents #ere once onelarge mass that $ro-e apart

885& process that ta-es place at midocean ridges

88=& part of molten roc- at midocean ridges

887& process of arth>s magnetic poles changing places

88?& items that provide evidence that the continents #ere once

closer together a& +eafloor spreading d& @agnetic minerals

$& 2ontinental drift e& fossils

c& @agnetic reversal


12/37

LESSON# %AIN PARTLESSON# %AIN PART

A E6plorin& t3e content te6t# reading eplaining and

learning voca$ulary and content concepts through

pictures videosand concept maps& (!5 minutes)

A C3ec1in& content te6t co'pre3ension# practicing

voca$ulary and language structures through a series

of activities& ("0 minutes)


13/37


THE THEORY

OF PLATE

TECTONICS

Ri&id plates of

roc-


14/37


earth%ua-es and

volcanoes occur incertain locations


15/37



16/37


PLATE !ONDARIES

a plate boundary


17/37


74 DI$ER(ENT

PLATE!ONDARY

https:// www.youtube.com/watch?v

=2q4Yqctq6nE

di*er&ent $oundary

%id8ocean rid&e in the


18/37


a ri-t *alley forms at


19/37


94 TRANSFOR% PLATE

!ONDARY

https:// www.youtube.com/watch?v

=1oLeKTvS!"

Eart3.ua1es

https://www.youtube.com/watch?v=1oLeKTvSIzQhttps://www.youtube.com/watch?v=1oLeKTvSIzQhttps://www.youtube.com/watch?v=1oLeKTvSIzQhttps://www.youtube.com/watch?v=1oLeKTvSIzQhttps://www.youtube.com/watch?v=1oLeKTvSIzQhttps://www.youtube.com/watch?v=1oLeKTvSIzQ


20/37


San Andreas-ault /one


21/37



22/37


:4 CON$ER(ENT PLATE!ONDARY

https:// www.youtube.com/watch?v=

K$%$L&!Yh'o

con*er&ent $oundary

t#o plates collide

The collision of t#o platesdeep ocean trenc3

T3e Rin& o- Fire

https://www.youtube.com/watch?v=KDrDLAzYhGohttps://www.youtube.com/watch?v=KDrDLAzYhGohttps://www.youtube.com/watch?v=KDrDLAzYhGohttps://www.youtube.com/watch?v=KDrDLAzYhGohttps://www.youtube.com/watch?v=KDrDLAzYhGohttps://www.youtube.com/watch?v=KDrDLAzYhGohttps://www.youtube.com/watch?v=KDrDLAzYhGo


23/37


:4 CON$ER(ENT

PLATE !ONDARY

the plate that is denseR

the process of subduction


24/37


Island arc Cslands of the *our @ountains partof


25/37


The colission of

urasian and Cndian plate resulted in

creation of Dimalayas&


26/37


PLATE %O$E%ENT

3ttps#;;

)))4youtube4co';)atc3<

*

=ryr>A(Y7d'E

The process of con*ection

2onvection currents

https://www.youtube.com/watch?v=ryrXAGY1dmEhttps://www.youtube.com/watch?v=ryrXAGY1dmEhttps://www.youtube.com/watch?v=ryrXAGY1dmEhttps://www.youtube.com/watch?v=ryrXAGY1dmEhttps://www.youtube.com/watch?v=ryrXAGY1dmEhttps://www.youtube.com/watch?v=ryrXAGY1dmEhttps://www.youtube.com/watch?v=ryrXAGY1dmEhttps://www.youtube.com/watch?v=ryrXAGY1dmE


27/37



28/37



29/37


The #ords in the right column match #ith the #ords in the left

column& *ind the #ord that doesn>t match&

RI(ID plates of roc- rules coffee discipline $ody procedure

DI$ER(ENT $oundaries thin-ing groups vie#s results eyes

DENSE plates forest clouds picture atmosphere fog

CON$ER(ENT $oundaries evidence validity thin-ing s-ills uice


30/37

LESSON# %AIN PART 0?@ %INTES2LESSON# %AIN PART 0?@ %INTES2

ACTI$ITIES 0:@ %INTES2ACTI$ITIES 0:@ %INTES2

A %atc3 t3e )ords )it3 pictures

1. a2 trans-or' boundary e2 con*ection currents

2. b2 con*er&ent boundary -2 'id8ocean rid&e

3. c2 di*er&ent boundary &2 oceanic trenc3


31/37


! %atc3 t3e )ords )it3 t3e de-initions#

ocean trenc3, di*er&ent, ri&id, subduction, con*ection currents

1& That separates or goes in different directions

& The movements of hot mantle roc- that drive tectonic plates in the process of convection&

!& < long narro# valley under the sea formed $y convergent $oundary

plate movement&

"& Dard not flei$le5& < process in #hich one plate slides under the other&


32/37


9 Loo1 at t3e te6t and -ind suitable )ords to -ill in t3e &aps in t3esentences belo)#

1& The t3eory o- plate tectonics states that arth>s surface is divided intorigid plates of roc-&

& The tectonic plates are pieces of crust and the upper part of the mantle&

!& The tectonic plates of the lithosphere 'o*e $ecause they rest on the fluidli-e astenosphere&

"& There are seven maor tectonic plates&

5& The /acific plate is the largest&

=& arth>s mantle 'o*es in the process of convection&

7& The plates are 'o*in& slo#ly&

?& The ;orth


33/37


: Fill in t3e &aps and t3en )rite t3e suitable )ords in t3e table belo)#


34/37


the largest

smaller

#armer

dense

colder


35/37


se t3e -ollo)in&

structures#

There #ill $e3

The plates #ill move3

The arth #ill loo- li-e

this3

The arth #ill not loo-

li-e3

C thin- that the plates

#ill move3 $ecause3


36/37

CLOSRECLOSRE


37/37

THAN+ YO FOR YORTHAN+ YO FOR YORATTENTIONATTENTION

The Theory of Plate Tectonics Ppt

Documents

Transcript of The Theory of Plate Tectonics Ppt