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Indian Stocks with Strong Dividend Potential in 2025 AI Powered Investment Plans ✌️【Stock Opportunities】✌️ Expert predictions with real-time stock indices, futures data, and metals, energy market data to help you seize the best investment opportunities. Thousands of years ago in the Himalayas, a river ate a smaller river and gave an unexpected boost to Everest’s height, scientists have discovered.
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“Our study shows how sudden changes in river systems can have far-reaching effects on landscapes,” said coauthorJin-Gen Dai, a professor of geology at China University of Geosciences in Beijing. “The main driver of Everest’s height remains the plate collision, but our discovery adds a new piece to this complex puzzle.”
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“Usually, rivers and mountains reach a kind of equilibrium, where erosion and uplift balance each other out,” Dai said. But when a river suddenly changes course, “it can shake things up dramatically. This sudden change can kick-start rapid erosion, which in turn triggers mountain uplift through isostatic rebound.”
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“This paper convincingly highlights the interplay of surface and deeper tectonic processes in shaping high topography on Earth,” Orme said in an email.
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Evidence of one ancient example still exists around the edges of the Himalayas, where long-ago river capture eroded deep gorges. This caused two regions — Namche Barwa in the east, and Nanga Parbat in the west — to rise about 0.2 to 0.4 inches (5 to 10 millimeters) per year, over millions of years, according to Orme. And today, in the Amazon drainage basin, “ongoing river capture is documented” and is thought to play a part in shaping the region’s steep topography.
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For the researchers, uncovering Everest’s growth spurt began with questions about the unusual course of the Arun. It currently flows from east to west along the northern Himalayas, draining a large area to the north of Everest, but then turns sharply to the south. In an expedition to the region, the scientists also found ancient lake sediments in the Arun River Basin, hinting at differences in water distribution millions of years ago.
“These features suggested that the upper and lower sections of the river may not have always been part of the same system,” Dai said. “This hinted at a past river capture event.”
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“Everest and its neighbors, which weren’t directly eroded by the river, got a free ride upwards,” Dai said.
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Compared with river piracy, erosion and uplift unspool over a much longer time span — and are still happening with Everest, Lhotse and Makalu.
“Calculating the exact duration of this rebound is challenging,” Dai said. “There’s still a lot of uncertainty in these calculations, especially regarding how long the isostatic rebound will continue.”
However, growth is just one part of Everest’s story. Even as the lingering effects of tectonic collision and the later rebound continue to push Everest upward, extreme weather and glacier movement are wearing the mountain down. For now, the researchers expect that Everest’s upward momentum will continue. But the mountain stands tall metaphorically, too — as a global icon and as a testament to the forces that shape our planet, Dai said.
“Understanding how it formed helps us grasp the bigger picture of Earth’s dynamic evolution,” he added. “As we face a future with changing climates and shifting weather patterns, understanding these processes could help us predict how our planet’s iconic landscapes might evolve in the future.”
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