Mount Everest, standing at 8.85 kilometres above sea level, continues to rise, according to a recent study published in Nature Geoscience. This iconic peak is not only the highest mountain on Earth but also a testament to our planet's dynamic nature.
The Himalayas have been elevating for around 50 million years due to the collision of the Indian and Eurasian tectonic plates. However, new research led by geoscientist Jin-Gen Dai from the China University of Geosciences reveals that Everest is growing even faster than previously anticipated. The study attributes this accelerated growth to a significant change in the region's river system.
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The research estimates that isostatic rebound contributes about 10% of Everest's annual uplift rate, equating to approximately 0.2 to 0.5 millimetres (0.01 to 0.02 inches) each year. Remarkably, this uplift exceeds the surface erosion caused by natural elements like wind, rain, and river flow.
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This study sheds light on the ever-changing nature of our planet, illustrating that even Mount Everest, a symbol of permanence, is shaped by geological processes. It serves as a reminder that the Earth is in constant flux, often in ways that go unnoticed in our daily lives.
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