Scientists finally find proof that Earth’s core is solid
Researchers from the Australian National University are confident they have found direct proof for the first time, that the Earth’s inner core is solid — albeit a little bit squishy, Newsweek reports.
In a paper published in the journal Science, Hrvoje Tkalčić, an associate professor, and Than-Son Phạm, a scholar, both at ANU, describe how they detected so-called “shear waves” or “J waves” in the inner core. These are a type of wave that can only travel through solid objects.
“We found the inner core is indeed solid, but we also found that it’s softer than previously thought.” – Hrvoje Tkalčić
Inner-core shear waves are so weak that they can’t be observed directly. In fact, detecting them has long been considered the “holy grail” of global seismology since scientists first predicted the center of the Earth was solid in the 1930s and 1940s.
The researchers used an approach that looked at the similarities between the signals at pairs of receivers after a major earthquake. This technique has been used by the same team to measure the thickness of the ice in Antarctica.
“Using a global network of stations, we take every single receiver pair and every single large earthquake — that’s many combinations — and we measure the similarity between the seismograms,” he said. “That’s called cross-correlation, or the measure of similarity. From those similarities we construct a global correlogram — a sort of fingerprint of the Earth.”
These results were used to demonstrate the existence of J waves and their speed in the inner core. Despite the new insights, there is much that remains a mystery about the center of the Earth.
“For instance, we don’t know yet what the exact temperature of the inner core is, what the age of the inner core is, or how quickly it solidifies, but with these new advances in global seismology, we are slowly getting there,” Tkalčić said.
WN.com, Jim Berrie
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