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Ayushree

The Himalayas originated from the Tethys geosyncline. Millions of years ago, a long, narrow, shallow sea called the Tethys existed between the northern Angaraland and southern Gondwanaland. As the Indian plate moved north, the sediments deposited in the Tethys were ...

Ayushree

The Himalayas are the definitive example of a Fold mountain. They were formed by the collision of the Indian and Eurasian plates. While the Nilgiri and Sahyadri (Western Ghats) are often considered structural plateaus or escarpments and the Satpura is ...

Ayushree

The Alps are Young Fold mountains, formed during the Tertiary period (roughly 30–65 million years ago). In contrast, the Urals and Appalachians are “Old Fold mountains” from the Paleozoic era and the Aravallis are one of the world’s oldest relict ...