A Moment of Science

Between A Hard Place And A Hard Place

Scientists armed with diamond anvils are pushing their investigations deeper and deeper into the center of Earth without actually having to go there.

EARTHCORE

Photo: SoylentGreen (Wikimedia Commons)

The ubiquity of cross-sectional diagrams like these gives the impression we have our planet's innards figured out. We're actually still working on it.

Given how much humanity has learned about the far reaches of space and the viscera of atoms, it may strike you as odd that a big, unsolved mystery could persist right under our feet.

But the fact is, geologists still don’t know exactly what Earth’s core is made of. 

Indirect Observation

Reasons for this lingering ignorance are twofold. First, we’d be burned up and crushed if we tried burrowing 1,800 miles down to observe the core firsthand. The heat and pressure are just too intense: neither our feeble bodies nor our tools could handle it.

(The world’s most penetrating mine, South Africa’s TauTona, is slightly more than two miles deep. Already at that depth, temperatures hover at a sweltering 130 °F!)

Second, the inward gravitational force of something as massive as Earth is staggering; scientists have been hard-pressed to recreate such conditions in the laboratory setting.

As a result of these empirical limitations, much of what we think we know about Earth’s internal composition and dynamics has had to be inferred indirectly from seismographic data. It’s like auscultation but with an entire planet instead of a single patient. Vibrations can only tell you so much.

Anvils Made Of Diamonds

Recently, however, researchers at Caltech have achieved pressure magnitudes equal to those of Earth’s outer core (around 171 gigapascals). And they didn’t even have to leave the climate-controlled comfort of the lab.

How? By squeezing a small sample of iron—the element thought to comprise much of Earth’s insides—between two tiny diamond anvils really, really, really hard.

Scientists hope analysis of iron’s properties under extreme duress will aid in our understanding not only of the core’s composition but of its formation and behavior.

Read More:

Ben Alford

Ben Alford works in Indiana Public Media's online dimension and holds an M.A. from Indiana University Bloomington's History and Philosophy of Science department. When not vegetating in front of a computer screen or geeking out over a good book, he can be found outside exploring.

View all posts by this author »

Stay Connected

What is RSS? RSS makes it possible to subscribe to a website's updates instead of visiting it by delivering new posts to your RSS reader automatically. Choose to receive some or all of the updates from A Moment of Science:

Support for Indiana Public Media Comes From

About A Moment of Science

Search A Moment of Science