The Himalayas have uplifted from which of the following geosynclines?

Key Points

• The Himalayas have uplifted from the Tethys geosynclines.
• The Tethys geosyncline was a large ancient ocean that existed between the continents of Gondwana and Laurasia before the uplift of the Himalayas.
• As the Indian Plate collided with the Eurasian Plate, the sediments in the Tethys geosyncline were compressed and uplifted, forming the Himalayan mountain range.
• This process is a prime example of orogeny, which is the structural deformation of the Earth's lithosphere due to tectonic plate interactions.

Additional Information

• The Himalayas are among the youngest mountain ranges in the world, estimated to have formed about 50 million years ago during the Cenozoic Era.
• The range is home to some of the planet's highest peaks, including Mount Everest, which stands at 8,848 meters (29,029 feet) above sea level.
• The formation of the Himalayas has had a significant impact on the climate and geology of the surrounding regions, influencing monsoon patterns and contributing to the rich biodiversity of the area.
• The ongoing tectonic activity in the region means that the Himalayas continue to rise, albeit at a slow rate.