October 3, 2024
3 min learn
How ‘River Piracy’ Helped Give Mount Everest a Progress Spurt
A mannequin suggests a large uplift attributable to a phenomenon referred to as “river piracy” partly explains Everest’s spectacular top
How did Mount Everest come to be the world’s tallest mountain, towering greater than 200 metres above the subsequent two highest peaks? Geologists counsel the mountain owes a part of its further top to 2 historic rivers that flowed via the Himalayas and merged about 89,000 years in the past. The ensuing erosion eliminated a lot rock and soil that Everest has rebounded upwards by as a lot as 50 metres, they are saying.
The outer crust of Earth responds to the removing of mass by slowly rising, says co-author Matt Fox, a geologist at College School London. “This has elevated the elevation of Everest.”
Everest, often known as Chomolungma and Sagarmāthā, stands 8,849 metres above sea degree, within the Himalayan mountain chain, which additionally accommodates the world’s third-highest peak, Kanchenjunga (8,586 metres) and isn’t removed from the second-highest, K2 (8,611 metres). The Himalayas have been pushed up by the ongoing collision of India with the remainder of Asia.
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Fox and his colleagues argue, in a research printed in Nature Geoscience at the moment, that a part of the reason for Everest’s excessive top lies within the close by Arun River.
Historical stream
The Arun rises north of the Himalayas however its course rapidly turns south, slicing a gorge via the mountains earlier than becoming a member of the massive Kosi River. “For 100 years, folks have puzzled why this river cuts via the tallest mountain ranges,” says Fox.
One risk is that the Arun was like that earlier than the Himalayas shaped. Nevertheless, many geologists suspect the Himalayas have been there first. They assume that the Arun as soon as had a special course, and that it eroded its manner via the mountains till it merged with a northerly river. This sort of occasion is called river seize or river piracy, says Fox.
“It may have been fairly a dramatic occasion,” says Fox. “It may need occurred throughout a time of flooding.”
Fox, working with colleagues together with Jin-Gen Dai, a geologist on the China College of Geosciences in Beijing, discovered that the Arun is a dramatic gorge with near-vertical sides in comparison with neighbouring rivers, suggesting it’s comparatively younger. They used fashions to simulate the attainable seize occasion, and located that it could have elevated erosion alongside the river’s path, explaining the bizarre channel.
The arguments for seize are fairly robust, says geologist Peter van der Beek on the College of Potsdam in Germany. “They clearly present it’s totally different from the opposite rivers,” he says, “and also you wouldn’t see that if it was a pre-existing river.” Earlier research have pointed to cases of river piracy elsewhere within the Himalayas, and to erosion alongside the Arun affecting close by mountains.
The staff’s best-fit mannequin means that the Arun seize occasion occurred 89,000 years in the past. Since then, the Arun has quickly eroded its channel, carrying away huge quantities of sediment. Launched from this mass, the crust may bob slowly upwards. The staff estimates that this ‘isostatic rebound’ has added between 15 and 50 metres to Everest’s elevation. Related mechanisms have been described earlier than, together with within the Himalayas.
Too simplistic?
Van der Beek is much less satisfied by these arguments. He says the timing of the river seize is unsure, as a result of the staff used a easy mannequin of river behaviour.
And the estimates of the mountain rising by 15–50 metres rely on the long-term charges of tectonic uplift and erosion, which aren’t nicely understood, he provides. That’s partly as a result of measurements of those charges return for just a few many years: not lengthy sufficient to incorporate dramatic seismic occasions. Van der Beek factors out that in 2015, a magnitude-7.8 earthquake in Nepal prompted many Himalayan mountains to subside by round 1 metre. Over lengthy timescales, a number of huge quakes can considerably have an effect on mountain top.
This text is reproduced with permission and was first printed on October 1, 2024.