Around 90 million years prior, during the late Cretaceous Period, the Indian Plate started moving north at around 15 cm/year (6 in/yr). Around 50 to 55 million years back, in the Eocene Epoch of the Cenozoic Era, the plate slammed into Asia in the wake of covering a separation of 2,000 to 3,000 km (1,243 to 1,864 mi), having moved quicker than some other known plate. In 2007, German geologists established that the Indian Plate had the option to move so rapidly in light of the fact that it is just half as thick as different plates which some time ago comprised Gondwanaland.
The impact with the Eurasian Plate along the advanced fringe among India and Nepal shaped the orogenic belt that made the Tibetan Plateau and the Himalayas. Starting at 2009, the Indian Plate is moving upper east at 5 cm/yr (2 in/yr), while the Eurasian Plate is moving north at just 2 cm/yr (0.8 in/yr). India is along these lines alluded to as the "quickest mainland".
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The country has four seasons: winter (January–February), summer (March–May), a rainstorm (stormy) season (June–September) and a post-rainstorm period (October–December).
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The country has four seasons: winter (January–February), summer (March–May), a rainstorm (stormy) season (June–September) and a post-rainstorm period (October–December).
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The Himalayas go about as a hindrance to the sub-zero katabatic breezes streaming down from Central Asia. Therefore, northern India is kept warm or just gently cooled during winter; in summer, a similar marvel makes India generally blistering.
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