By Strange Sounds
Apr 4, 2021
In the case of the central Alps, the situation is scientifically complex. First, a rapid review of the basics of plate tectonics: Earth is basically a floating ball of slick magma with a thin candy shell of crust around the outside. The crust is broken into large parts, and these parts continue to push into and crunch away at each other.
This causes different things — not just earthquakes and volcanoes, but also continental drift and the consequent destruction and recreation of crust. Deep within the Atlantic Ocean, new ocean floor emerges every day as the two sides are pushed apart. On the other end, ocean floor collides with and is pushed beneath the continental plates.
So imagine filling your bathtub with cold water and then dropping in enough big chunks of ice to fill the surface and then some. The chunks will start to push each other and rise and fall. This is exactly what happens in the crust, and it’s why the Alps are still growing.
It’s called crustal uplift, crustal uprise, tectonic uplift—all terms that refer to the same idea. And after thinking about how Earth’s crust roams and interacts, it’s easy to see why deciding how to measure the height of these mountains is itself a challenging problem.
In this case, any crustal uplift is working against the related up-top phenomenon of erosion. The Alps are, cosmologically speaking, just babies compared to many of the world’s oldest mountain ranges. Because of that, they’re still spiky and jagged, extremely tall, and subject to high rates of erosion at their peaks.
Scientists have long believed the Alps are basically shifting in place like an escalator: uplifted by the crust and eroded from the top at the same rate. They can use chemical signatures made by bouncing cosmic radiation to estimate how much of what’s visible at the very top of a mountain is very old and, therefore, the result of erosion of the newer rock over top—like the shiny nose on a much-beloved local statue rubbed for good luck.
“As cosmic rays hit Earth’s surface, oxygen atoms that constitute quartz minerals experience a nuclear reaction,” scientists from Bern University explain in a statement. “[A] new isotope is formed. Because [it’s] only formed on Earth’s uppermost surface, the surface age can be determined with this isotope. If the concentration is high, then the surface has been exposed to cosmic rays for a relatively long time and is therefore relatively old.”
The scientists found that erosion is slower than crustal uplift, especially in Switzerland, where the Alps erode at an astonishing 14 millimeters per 1,000 years. Uplift, on the other hand, can be as high as 800 millimeters during the same time frame. These parts of the Alps are racing upward more than 50 times faster than they’re sanded down.
Understanding the difference can help scientists make more accurate measurements of other phenomena, including in detailed studies of why and where erosion happens the most. More Information Here!!