Concepts



Quick concepts:

What humans know

  1. Some earthquake (seismic) waves travel THROUGH the Earth, as well as along its surface.

  2. Seismic waves are a type of mechnical (rather than electromagnetic) wave and thus require an intervening medium to propagate (move through).
  3. Mechanical waves such as earthquake waves travel through materials at different velocities depending on properties of materials.

  4. At boundaries between materials of different properties, earthquake waves bend and change direction of travel.

  5. The more time elapsed, the further away the front of an earthquake wave gets from its source.

  6. P (primary or compressional)and S (secondary or shear) waves generally travel faster through solids that are more dense.

  7. S (shear) waves cannot travel through liquids.

Quick facts:

How do we know it?

  1. Scientists use earthquake (seismic) waves to look inside the Earth to determine the depth boundaries between different layers of rock.

  2. Scientists occasionally get to look at the composition of materials that escape from the interior of the planet when it comes out of volcanoes.

  3. Most material that erupts out of a volcano does not come from very deep inside the Earth.

  4. In rare places, we can see pieces of the upper mantle in person where they have been pushed to the Earth's surface by tectonic forces in unusual circumstances.

  5. Scientists make "educated" guesses about the composition and existence of layers by considering multiple lines of evidence - such as the strength of the Earth's gravitational field, and the composition of the Earth compared with the composition of other objects in our solar system such as meteorites.


Practical matters:

Why is it important to know?

  1. Knowing what lies underneath the surface of the Earth helps us figure out why the plates move at the surface and why volcanoes erupt in certain places.
  2. Knowing how to use seismic waves to image the interior of the Earth helps us similar technologies to buried natural resources such as oil and gas.
  3. Knowing how to use seismic waves to image the interior of the Earth helps us spot hazards such as faults where earthquakes might occur.
  4. Knowing about the interior of our own planet lets us compare the Earth with other planets and understand the special conditions that make it our home.