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unistudentguy unistudentguy
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6 years ago

Why do we know that the geothermal gradient near the surface cannot continue very deeply into
  Earth? What will be an ideal response?





Q. 2 -

What is Earth's average density, what are the average surface rock densities, and what does this tell us
  about the interior of Earth? What will be an ideal response?





Q. 3 - What evidence do scientists use to estimate the density and composition of the core? What will be an ideal response?



Q. 4 - Why are the paths of seismic waves curved? What will be an ideal response?
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Replies
wrote...
6 years ago
(Answer to question 1 )  

If the geothermal gradient near the surface continued at depth, the temperature at only 100 km depth
would be so high that all known rocks would melt despite the high pressure.



(Answer to question 2 )  

Earth's average density is 5.5 g/cm3, surface rocks range between 2.5 and 3.0 g/cm3, and, therefore, the
interior must be denser than the crust.



(Answer to question 3 )  

The composition of the core is estimated by studying the composition of meteorites, information from
seismic waves, laboratory experiments, and Earth's density.



(Answer to question 4 )  Density and elasticity vary with depth, causing the waves to be continually refracted.
unistudentguy Author
wrote...
6 years ago
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