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 Home » Tutorials » Geography » Physical Geography » Origin of Continents and Oceans

Origin of Continents and Oceans


A D V E R T I S E M E N T
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The present distribution of the continents has taken place in the last 65 million years. The drift of continents still continues. The ridges down the middle of ocean floors have been emitting lava actively.

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A D V E R T I S E M E N T


These midoceanic ridges, are cracks on the floor of ocean where molten rocks push up to form new crust. The crust spreads away from the ridge and the ocean basin widens. This phenomena is known as Sea Floor Spreading. The Atlantic Ocean is getting wider by several centimetres a year, the Pacific Ocean is getting smaller, and the Red Sea is part of a crack in the crust that will widen to produce a new ocean millions of years in future. The widening South Atlantic Ocean has separated Africa and South America.

PLATE THEORY



According to the global plate tectonic theory, the lithosphere is broken into a number of moderately rigid plates. The plates move continuously and have relative direction of motion. Based on the relative motion of plates, three kinds of plate boundaries or marginal zones are recognised �

(i) zones or margins of divergence or spreading;

(ii) zones or margins of convergence; and

(iii) fracture zones or transform faults.

Zones of divergence are boundaries along which plates separate and in this process of separation molten material upwells. This is commonly observed along linear ocean ridges where new lithosphere is created in the form of new ocean floors. Active volcanism and shallow focus earthquakes mark such boundaries. Zones of convergence are boundaries along which the edge of one plate overrides the other. The overridden plate slips down into the mantle and is absorbed. This process is known as subduction. Besides volcanism and shallow to deep focus earthquakes, these boundaries also produce deep trenches/ basins and folded mountain chains. There is neither creation nor destruction along the transform fault. The lithospheric plates slide past each other.





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