1. Mount Everest is located in the Himalayas at the boundary of the In...
Formation of Mount Everest:
Mount Everest was formed due to the collision of the Indian and Eurasian tectonic plates. The Indian plate, moving northwards, collided with the Eurasian plate, causing the Earth's crust to fold and push upwards. This process, known as continental collision, led to the formation of the Himalayan mountain range, with Mount Everest being the tallest peak.
Increasing Height of Mount Everest:
Mount Everest's height is increasing every year due to geological processes such as tectonic uplift and erosion.
- Tectonic Uplift: The ongoing collision of the Indian and Eurasian plates continues to push Mount Everest upwards at a rate of about 4 mm per year. This slow but steady movement contributes to the mountain's increasing height over time.
- Erosion: While tectonic uplift plays a significant role in the growth of Mount Everest, erosion also plays a part in shaping the mountain. The forces of weathering, glacial movement, and other erosional processes wear down the mountain's surface, but the tectonic uplift counteracts this erosion by continually pushing the mountain upwards.
- Overall Impact: The combination of tectonic uplift and erosion results in a net increase in Mount Everest's height each year. This process has been ongoing for millions of years, contributing to the mountain's current height of 8,848 meters (29,029 feet) above sea level.
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