0
What else can I help you with?
Who discovered Earth's inner core?
The Danish geophysicist Inge Lehmann discovered Earth's inner core in 1936.
Who discovered the inner core?
The Danish geophysicist Inge Lehmann discovered Earth's inner core in 1936
How was the earth's core discovered?
The existence of a solid inner core distinct from the liquid outer core was discovered in 1936 by seismologist Inge Lehmann
Who discovered Earth's core?
The British geologist Richard Dixon Oldham discovered the Earth's core and published his results in 1906.
Who discovered the Outer Core?
The outer core of the Earth was indirectly discovered by detecting seismic waves that travel through it. Scientists used data from earthquakes and seismic waves to infer the existence and properties of the outer core, which lies beneath the mantle.
How was Earth's core discovered?
By studying how seismic waves travel through the Earth's interior.
Who discover inner core?
The Danish geophysicist Inge Lehmann discovered Earth's inner core in 1936
By studying earthquake waves scientists have discovered that earth's core has two parts true or false?
True, honey! Scientists have indeed discovered that the Earth's core has two parts by studying earthquake waves. We've got the inner core, which is solid as a rock, and the outer core, which is liquid and sloshing around like a lava lamp. So, buckle up, buttercup, because the Earth's core is a wild ride of hot messiness!
What is Inge lehman contribution?
Inge Lehman, a Danish scientist, discovered the solid core of the Earth.
Have scientist discovered all of earth's organisms why or why not?
no body knows becasue there could be tiny organisms or even live in the earth's core
What is named after the German geologist that discovered the thing that separates the earth's mantle from the outer core?
the Gutenberg discontinuity
How did scientists find out about earth's core has two parts?
Scientists discovered that Earth's core has two parts—a solid inner core and a liquid outer core—through the study of seismic waves generated by earthquakes. By analyzing how these waves travel through the Earth, they observed that certain waves could pass through the outer core but were reflected by the inner core, indicating different states of matter. Additionally, the behavior of these waves provided insights into the core's composition and physical properties. This research was pivotal in understanding the Earth's internal structure.
