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Tiny crystals capture millions of years of mountain range history – a geologist excavates the Himalayas with a microscope
By Matthew J. Kohn, Boise State University
The Himalayas stand as Earth’s highest mountain range, possibly the highest ever. How did it form? Why is it so tall?
You might think understanding big mountain ranges requires big measurements – perhaps satellite imaging over tens or hundreds of thousands of square miles. Although scientists certainly use satellite data, many of us, including me, study the biggest of mountain ranges by relying on the smallest of measurements in tiny minerals that grew as the mountain range formed.
These minerals are found in metamorphic rocks – rocks transformed by heat, pressure or both. One of the great joys in studying metamorphic rocks lies in microanalysis of their minerals. With measurements on scales smaller than the thickness of a human hair, we can unlock the age and chemical compositions hidden inside tiny crystals to understand processes occurring on a colossal scale.
Measuring radioactive elements
Minerals containing radioactive elements are of special interest because these elements, called parents, decay at known rates to form stable elements, called daughters. By measuring the ratio of parent to daughter, we can determine how old a mineral is.
With microanalysis, we can even measure different ages in different parts of a crystal to determine different growth stages. By linking the chemistry of different zones within a mineral to events in the history of a mountain range, researchers can infer how the mountain range was assembled and how quickly.
My research team and I analyzed and imaged a single grain of metamorphic monazite from rocks we collected from the Annapurna region of central Nepal. Though only 0.07 inches (1.75 mm) long, this is a gigantic crystal by geologists standards – roughly 30 times larger than typical monazite crystals. We nicknamed it “Monzilla.”
Using an electron probe microanalyzer, we collected and visualized data on the concentration of thorium – a radioactive element, similar to uranium – in the crystal.