who discover the following Gutenbergdiscontinuity
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The discontinuity was discovered by Beno Gutenberg (1889-1960), a seismologist who made several important contributions to the study and understanding of the Earth's interior. The CMB has also been referred to as the Gutenberg discontinuity, the Oldham-Gutenberg discontinuity, or the Wiechert-Gutenberg discontinuity.
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The Gutenberg Discontinuity is situated at a distance of 2900 kilometres beneath the earth's surface. It is named after Andriza Mohorovicic, who discovered it. It is named after Beno Gutenberg, who discovered it.
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