The northward drift of the Indo-Australian plate resulted in its collision with the much larger Eurasian plate. Which of the following was the result of this collision?
According to the Theory of Plate
Tectonics, the Earth’s crust was initially a single, giant super-continent
called Pangea. Its northern part was the Angara land and the southern part was
the Gondwana land. The movement of the molten material below the Earth’s crust
caused the crust to break up into a number of large
fragments called lithospheric or tectonic plates. Another important feature of
the Earth’s crust at the time was the geosyncline — a narrow, shallow, elongated
basin with a sinking bottom in which a considerable thickness of sediments were
deposited by the rivers coming from Angara land and Gondwana land — called the
Tethys. After separating from the Gondwana land, the Indo-Australian Plate
drifted towards the north in the direction of the Eurasian Plate. This resulted
in the collision of the two plates, and due to this collision, the sedimentary
rocks in the Tethys got folded to form the mountain system of western Asia and
the Himalayas.