power point

17
MANNAM FOUNDATION CENTRE FOR EDUCATION TECHNOLOGY (Recognized by NCTE and affiliated to the University of Kerala) PORUVAZHY, EDAKKAD P.O, KOLLAM POWER POINT PRESENTATION SEMESTER –II B.Ed. COURSE 2014-15 NAME OF THE STUDENT TEACHER : AISWARYA RAJ. L SUBJECT: SOCIAL SCIENCE CANDIDATE CODE : 16914373001 Certified Record of ………………………..................................................…………… Candidate Code: ………....................……..............…….........…….. for the year 2014-15 Examiner Lecturer Principal

Upload: softislandsolutions

Post on 13-Apr-2017

146 views

Category:

Career


0 download

TRANSCRIPT

Page 1: Power point

MANNAM FOUNDATIONCENTRE FOR EDUCATION TECHNOLOGY

(Recognized by NCTE and affiliated to the University of Kerala)PORUVAZHY, EDAKKAD P.O, KOLLAM

POWER POINT PRESENTATION

SEMESTER –II

B.Ed. COURSE 2014-15

NAME OF THE STUDENT TEACHER : AISWARYA RAJ. LSUBJECT : SOCIAL SCIENCECANDIDATE CODE : 16914373001 

Certified Record of ………………………..................................................……………

Candidate Code: ………....................……..............…….........…….. for the year 2014-15

ExaminerLecturer Principal

Page 2: Power point
Page 3: Power point

PRESENTED BY,

AISWARYA RAJ LSOCIAL SCIENCE

REG NO : 16914373001

Page 4: Power point

MANNAM FOUNDATION CENTRE FOR EDUCATIONAL

TECHNOLOGY.PORUVAZHY, EDAKKAD

P.O., KOLLAM.

Page 5: Power point
Page 6: Power point

Composition ( what it is made of)

Crust Mantle Core

The Earth is divided into three layers based upon the material it contains.

Page 7: Power point

The Crust The comparatively thin outer shell of the Earth. Approximately 40 km thick. Two parts- continental crust, oceanic crust. As silica and alumina are the chief contents, the continental crust is also known

as SIAL. As silica and magnesium are the chief

contents, the oceanic crust is also known as SIMA

Page 8: Power point

Oceanic and continental crust

Oceanic crust is thin but very dense.

Page 9: Power point

The Mantle Located beneath the crust. Extends up 2900 km from the the crust. Tow parts- upper mantle, lower mantle. The upper mantle, made up silicon compounds, is in a solid state. The lower mantle, located beneath the

upper mantle, is in a semi-liquid state.

Page 10: Power point

The Core Central part of the Earth. From 2900 km to 6371km. Two parts- outer core, inner core Due to the high pressure prevailing at the centre, the inner core is in a solid state. The materials in the outer core are in a

molten state. It is mainly made up of the minerals nickel

(Ni) and iron (Fe), it is also known as NIFE.

Page 11: Power point
Page 12: Power point

A new way to divide the Earth

The Earth is also divided up into layers based upon the physical properties of each layer. Lithosphere Asthenosphere Mesosphere Outer core Inner core

Page 13: Power point

Physical structure of the Earth ( 5 Layers )

Lithosphere :- Rigid outer layer ( crust and part of the mantle). Asthenosphere :- Soil rock that flows slowly, found below lithosphere like frosting part of the mantle . Mesosphere :- Middle layer, part of the mantle very rigid magma. Outer core :- Liquid layer. Inner core :- Solid, very dense.

Page 14: Power point
Page 15: Power point
Page 16: Power point

Tectonic plates

Earth’s crust is broken into about 19 pieces. The plates move on top of the

asthenosphere.

Page 17: Power point