Science & technology

Inge Lehmann discovers the Earth's inner core

1936

Studying seismograms of earthquakes in New Zealand, the Danish seismologist Inge Lehmann noticed seismic waves arriving where none should be if the Earth's core were a single liquid ball. In 1936 she concluded that there is a solid inner core inside the liquid outer core, with a radius of about 1,200 km. Her paper, only a few pages long and titled simply 'P prime', was confirmed in the 1970s by computer analysis. The inner core, mostly iron and nickel, is about as hot as the surface of the Sun.

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