Danish scientist Inge Lehmann discovered Earth's solid inner core in 1929 by analyzing seismic waves from a New Zealand earthquake, noticing that some waves bent and bounced in ways that indicated a solid inner core surrounded by a liquid outer core; modern scientists later confirmed this discovery and found that Earth's inner core rotates at a different speed than the surface, following a roughly 70-year cycle of speeding up and slowing down.
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Deep Dive
How We Discovered Earth’s Hidden Solid Core #spacesuccess #rain #siliceous #innercore #universeAdded:
The day the deepest hole humans ever dug reaches only about 2/10 of a percent toward Earth's center.
So, how did we uncover Earth's molten oceanic [music] interior? But in 1929, a huge earthquake in New Zealand changed everything.
The quake sent seismic waves racing through the Earth in every direction.
Danish scientist Inge Lehmann studied those waves [music] carefully and noticed something strange.
Some waves were bending and bouncing in ways they shouldn't. After doing the math, Lehmann realized the only explanation was this.
Inside Earth's [music] liquid outer core, there had to be a solid inner core.
Modern scientists later confirmed her discovery using advanced computers and highly sensitive seismic recordings. And they uncovered something even more shocking.
Earth's inner core rotates at a different speed than the surface above us.
Scientists now [music] think the core follows a roughly 70-year cycle of speeding up and slowing down.
And right now, it may actually be slowing down. A hidden metal sphere spinning beneath our feet, discovered without ever [music] seeing it directly.
A testament to human curiosity.
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