Scientists Detect Shape-Shifting Along Earth’s Solid Inner Core
Scientists of course cannot cut into Earth and directly observe its insides. Instead, their knowledge is inferred from the vibrations generated by earthquakes that pass through the planet. The speed and the direction of the seismic vibrations change depending on the density and the elasticity of the rocks.
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As you might have guessed, given that Hough is a seismologist for the USGS, the study she and her team recently published in ...
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Unexpected ocean find rewrites Earth's geological timelineScientists have identified an anomaly linked to the rise in beryllium-10 levels in ocean sediments on the Pacific Ocean floor ...
Scientists at Yale and in Singapore have devised what may be the ultimate acid test—a comprehensive model for estimating the ...
The ocean plate was once the seafloor of Neotethys — an ocean that formed when the supercontinent Pangaea broke up into a ...
The highest potential for naturally occurring hydrogen is in the Midcontinent Rift system, which runs through central parts ...
"It's pretty surreal to walk between two major pieces of Earth's crust that are drifting in different directions," Brooke ...
Yellowstone Caldera Chronicles is a weekly column written by scientists and collaborators of the Yellowstone Volcano Observatory. This week's contribution is from Cathy Whitlock, Regents Professor ...
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