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Why Some Mountain Ranges Stick Around

Elevation map of ancient topography in the southern Ural Mountains in Russia.
Elevation map of ancient topography in the southern Ural Mountains in Russia.
(Image credit: David Lundbek Egholm)

Landslides, or the lack thereof, may help mountain ranges remain far longer than previously thought, new research suggests.

As the tectonic plates that make up Earth's surface drift, mountain ranges such as the Himalayas in Asia and the Andes in South America form where the plates collide, similar to the way car bodies crumple during crashes. In the absence of such mountain-building tectonic activity, mountain belts are expected to slowly erode over time due to forces such as rain and glaciers.

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Charles Q. Choi
Live Science Contributor
Charles Q. Choi is a contributing writer for Live Science and Space.com. He covers all things human origins and astronomy as well as physics, animals and general science topics. Charles has a Master of Arts degree from the University of Missouri-Columbia, School of Journalism and a Bachelor of Arts degree from the University of South Florida. Charles has visited every continent on Earth, drinking rancid yak butter tea in Lhasa, snorkeling with sea lions in the Galapagos and even climbing an iceberg in Antarctica.