Data captured from seismic waves caused by earthquakes has shed new light on the deepest parts of Earth’s inner core, according to seismologists from The Australian National University (ANU).
Data captured from seismic waves caused by earthquakes has shed new light on the deepest parts of Earth’s inner core, according to seismologists from The Australian National University (ANU).
By measuring the different speeds at which these waves penetrate and pass through the Earth’s inner core, the researchers believe they’ve documented evidence of a distinct layer inside Earth known as the innermost inner core – a solid ‘metallic ball’ that sits within the centre of the inner core.
Not long ago it was thought Earth’s structure comprised four distinct layers: the crust, the mantle, the outer core and the inner core. The findings, published in Nature Communications, confirm there is a fifth layer.
“The existence of an internal metallic ball within the inner core, the innermost inner core, was hypothesised about 20 years ago. We now provide another line of evidence to prove the hypothesis,” Dr Thanh-Son Phạm, from the ANU Research School of Earth Sciences, said.
Read more at Australian National University
Image: Professor Hrvoje Tkalčić. (Photo: Jamie Kidston/ANU)
