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Whose discovery of seismic waves transformed the study of earthquakes?

GeophysicsSeismology

Quick Answer

Beno Gutenberg is credited with major advances in seismology, including identifying Earth's core boundary in 1914. His work helped make earthquake waves a tool for studying Earth's interior.

The Full Story

German-American seismologist Beno Gutenberg made foundational contributions to understanding how earthquake waves travel through Earth. In 1914, he determined the depth of the Earth's core-mantle boundary, now called the Gutenberg discontinuity, at about 2,900 kilometres. That discovery came from analysing the paths of seismic waves from earthquakes. Gutenberg's work showed that earthquakes are not only destructive events but also probes of Earth's interior structure. His research remains central to modern seismology.

Key Facts

1.The Gutenberg discontinuity is about 2,900 km deep
2.Beno Gutenberg identified it in 1914
3.Seismic waves reveal Earth's interior structure

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Suggested video title for this topic:

"Earthquakes became X-rays for the planet—thanks to one scientist."