Monday 8 December 2014

Smart Notes on world geography (Physical) part - 3

Today we have discussed about the different theories proving the origin of continents and basins
If you will look at the syllabus you will find that in GS – 1, there is section namely important geographical phenomenon.
So the upcoming modules will be titled as important geographical phenomenon, where we would cover every aspects of world geography namely physical, social and economic.
We would cover all conceptual aspects under this module,


Important geographical phenomenon
1.       In order to understand important geographical phenomenon of geography, as per the syllabus of GS it is necessary to understand the origin of continents and ocean basins.
2.       Continent and ocean basins are fundamental relief feature of the globe.
3.       They are considered as relief features of the first order, and different theories regarding the origin of the continents and oceans are being put forth by the scientists.
4.       About 70.8 percent of the total surface area of the globe is represented by the oceans and 29.2 are represented by the continents.
Distributional pattern of the continents and ocean basins
1.       There is overwhelming dominance of land areas in the northern hemisphere; more than 75% of total globe is situated to the north of the equator.
2.       Continents are arranged in roughly triangular shape; most have their bases (of triangle) in the north while their apices are pointed towards south.
3.       The oceans are also triangular in shape, contrary to the continents the base of oceans is in the south while their apices are in the north.
4.       The North Pole is surrounded by oceanic water, while South Pole is surrounded by land area (of the Antarctic Ocean).
5.       There is antipodal situation of continents and oceans, only 44.6 percent oceans are situated opposite to oceans.
6.       1.4 percent of the total land area of the globe is opposite to land area; more than 95% of the total land area is situated opposite to water bodies.
7.       The great Pacific Ocean basin occupies almost one – third of the entire surface area of the globe.
The above mentioned characteristic would help us to validate the authenticity of any hypothesis or theory dealing with the origin and evolution of the continents and ocean basins.
There are various hypotheses regarding the origin of the earth, but we would discuss the following one, they are considered to be much more scientific.
1.       Tetrahedral hypothesis postulated by Lowthian Green
2.       Continental drift theory of Taylor
3.       Plate tectonic theory
4.       Sea floor spreading

Tetrahedral hypothesis
1.       It is based on the fundamental principles of geometry
2.       Elie de Beaumont is considered to be first the attempted in this field
3.       But the theory of Lowthain (in 1875) is most significant of all hypotheses based on geometric principles.
4.       He based his hypothesis on the two basic principle of geometry
                             (i) A sphere is that which contains the largest volume with respect to its surface area
                            (ii) A tetrahedron is that body which contains the largest volume with respect to its      surface area.
Basic assumption
1.       It is based on the characteristics of a tetrahedron which is a solid body having four equal plane surfaces.
2.       Each of which is an equilateral triangle. He postulated it after considering the characteristics of the distributional pattern of the land and water over the globe.
3.       There is dominance of land area in the northern hemisphere and water areas in the southern hemisphere
4.       Triangular shape of continent and oceans,
5.       Situation of continuous ring of land around north polar sea and location of south pole in land area (Antarctica) surrounded by water from all sides
6.       Antipodal arrangement of continent and oceans
7.       Largest extent of Pacific Ocean covering one third area of the globe
8.       Location of chain folded mountains around Pacific Ocean.
9.       According to him when earth was originated it was in sphere form
10.   In the beginning earth was very hot but it gradually began to cool down due to loss of heat.
11.   First the quarter part of the earth cooled down and thus was formed the crust but the inner part was continued to cool down
12.   Consequently the inner part of the earth was subjected to much more contraction, thus there was marked reduction in the inner part of the earth.
13.   Upper part of the earth (crust) was already cooled down, and could not be subjected to further contraction.
14.   This resulted into possible gap between the upper and inner parts of the earth.
15.   Consequently the upper part collapsed on the inner part and ultimately the earth began to assume the shape of a tetrahedron.
16.   He also clarified that due to structural variations; there may be some deviations from a true tetrahedron.
17.   Four oceans (the Pacific Ocean, the Atlantic Ocean, the Indian Ocean and the Arctic Ocean) were created on the four plane faces of the terrestrial tetrahedron.
18.   These plane faces retain water because of the fact that these were lower than the level of the apices or coigns of the terrestrial tetrahedron.

Fig- Distribution of land and water on a tetrahedron
Criticism
1.       To major extent it successfully explains the characteristics feature of the distributional pattern of the present day continents and ocean basin.
2.       But because of certain basic defects and errors the theory is not acceptable to the modern scientific community.
3.       It is argued that balance of the earth in the form of a tetrahedron while rotating on an apex cannot be maintained.
4.       The earth rotating so rapidly on its axis that the spherical earth cannot be converted into a tetrahedron while contracting on cooling.
5.       This hypothesis believes more or less in the permanency of continents and ocean basins, while plate tectonic theory has validated the concept of continental drift.

Continental drift theory of Taylor
1.       F.B .Taylor postulated his concept of horizontal displacement of the continents in 1908.
2.       The main purpose of his hypothesis was to explain the problems of the origin of the folded mountains of tertiary period.
3.       The concept of Taylor is considered to be the first attempt in the field of continental drift, though Antonio Snider presented his views about drift in the year 1858 in France.
Basic Assumption
1.       According to him there were two land masses during Cretaceous period.
2.       Lauratia and Gondwanaland were located near the north and south pole respectively.
3.       The continent were made of sial which was practically absent in the oceanic crust.
4.       Continent moved towards the equator, the main driving force of the continental drift was tidal force.
5.       Continents were displaced in two ways:
                                           (i) Equator wards movement
                                           (ii) Westward movement
Hypothesis
1.       Lauratia started moving away from the North Pole because of enormous tidal force of the moon towards the equator in a radial manner.
2.       This movement of landmass resulted into tensional force near the north pole which caused stretching, splitting and rupture in landmass.
3.       The displacement of the Gondwana land from the South Pole towards the equator caused splitting and disruption.
4.       Arctic sea was formed between Greenland and Serbia due to earthward movement of Lauratia.
5.       Atlantic and Indian Ocean were supposed to have been formed because of filling of gaps between the drifting continents with water.
6.       Taylor assumed that the landmasses began to move in the lobe form while drifting through the zones of lesser resistance.
7.       Thus mountain and island arcs were formed in the frontal part of the moving lobes.
8.       The Himalayas. Caucasus and Alps are considered to have been formed during equator ward movement of the Lauratia and Gondwanaland from the  north and south poles respectively
9.       The Rockies and Andes formed due to westward movement of the landmasses.
Criticisms
1.       Taylor’s main aim was to explain the origin of the tertiary folded mountains and hence he made the continents to move at a very large scale.
2.       He described displacement of the landmasses for thousands of kilometres, but displacement of landmasses up to 32-64 Km would have been sufficient enough for the purpose.
3.       Tidal force was used as mode of displacement , if it was so enormous during cretaceous period that it could displace the landmasses for thousands of kilometres
4.       Apart then it might have also put a break on the rotatory motion of the earth and thus rotation of the earth might have been stopped within a year.
5.       Though the concept of F.B. Taylor is not acceptable but his hypothesis is considered to be significant on the ground that
6.       He raised his voice very forcefully through deductive postulation against the prevalent concept of the permanency of the continents and ocean basins.


 Plate tectonic theory
1.       It was a great scientific achievement of the decade of 1960s; it is based on the two major scientific concepts
                                         (i) The concept of continental drift
                                         (ii) The concept of sea – floor spreading
2.       Lithosphere is internally made of rigid plates (first used by Canadian geophysicist J.T. Wilson in 1965), six major plates and 20 minor plates have been identified so far.
3.       Six major plates are Eurasian plate, Indian – Australian plate, American plate, Pacific plate, African plate and Antarctic plate.
4.       W.J.Morgan and Le Pichon elaborated the various aspects of plate tectonics in 1968
5.       Now the continental drift and the displacement are considered a reality on the basis of plate tectonics.
6.       Tectonic plate boundaries are most important because all tectonic activities occur along the plate margins.

Fig- Main aspects of plate tectonics
Plate margins are generally divided into three groups
Constructive plate margins
1.       These are also called divergent plate margins or accreting plate margins.
2.       It represents zone of divergence where there is continuous upwelling of molten material (lava) and thus new oceanic crust is continuously formed.
Destructive plate margins
1.       These are also called as consuming plate margins or convergent plate margins.
2.       Two plates move towards each other or two plates converge along a line and leading edge of one plate overrides the other plate.
3.       The overridden plate is sub ducted or thrust into the mantle and thus part of the crust (plate) is lost in the mantle.
Conservative plate margins
1.       These are also called as shear plate margins
2.       Two plates pass or slide past one another along a transform faults and thus crust is neither created nor destroyed.

Fig- Different types of plate margins
Conclusion
1.       H. Hess postulated the concept of plate tectonics in 1960, in support of continental drift.
2.       The continents and ocean move with the movement of these plates.
3.       The present shape and arrangement of continent and ocean basins could be attained because of continuous movement of different plates.
4.       Plate tectonic theory is based on the evidences of sea floor spreading and palaeomagnetism .


Sea – floor spreading
1.       Propounded by the Harry Hess of the Princeton University in the year 1960.
2.       He propounded that mid – oceanic ridges were situated on the rising thermal convection currents, coming up from the mantle.
3.       The oceanic crust move in opposite directions from mid – oceanic ridges.
4.       This molten lava cool down and solidify to form new crust along the trailing ends of divergent plates (oceanic crust).
5.       Thus there is continuous creation of new crust along the mid – oceanic ridges and the expanding crusts (plates) are destroyed along the oceanic trenches.
6.       These facts prove that continents and ocean basins are in constant motion.



Fig – pattern of thermal connective currents and plate movements

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