Erosion caused by glaciation during ice ages can, in the right circumstances, wear down mountains faster than plate tectonics can build them, the researchers said.
The study has given an insight into how climate tectonic forcesand climate tectonic forces influence mountain building over a prolonged period of time.
The study, conducted by a team of scientists from 10 countries including the University of Exeter in UK, attempted to measure all the material that left and entered the St Elias Mountain range, on the Alaskan coast, over the past five million years, using seismic imaging equipment and marine coring. The researchers imaged and mapped a huge fan of sediment in the deep sea.
The new research, which is the product of the culmination more than a decade of field work, has shown that mountain ranges actively evolve with, and respond to, Earth's climate, rather than being static, unyielding parts of the landscape.
"It turned out most sediments were younger than we anticipated, and most rates of sediment production and thus erosion were higher than we anticipated," said Sean Gulick, co-chief scientist from the University of Texas.
"Since the big climate change during the mid-Pleistocene transition when we switched from short (about 40,000-year) ice ages to super long (about 100,000-year) ice ages, erosion became much greater. In fact, there was more erosion than tectonics has replaced," he added.
Mountain ranges form when tectonic plates thrust into one another over millions of years and scrunch up Earth's outer crust. But even as mountains are built by these titanic forces, other agents - some combination of tectonic and climate processes - work to remove the accumulating crust.
The study highlights the pivotal role climate Mfluctuations play in shaping Earth's landforms. The findings were published in the journal Proceedings of the National Academy of Sciences.


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