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19 Cards in this Set

  • Front
  • Back

Elemental composition of the Earth

Iron 35%,


Oxygen 30%,


Silicon 15%,


Magnesium 10%

Makes up most rock

Silicate SiO2

Rate of change in temp with depth in Earth


Geothermal Gradient

Using Earthquake waves to see inside Earth

Seismology

First wave in an earthquake

P Wave

Similar to soundwaves, pushes and pulls

P Wave

Travels through rock and liquids

P Wave

Arrives later than P waves

S Wave

Shears rock sideways or up and down

S Wave

Only travels through solids

S Wave

Used to show direction and speed of waves

Rays

Waves do this when crossing different densities in earth

Reflect or Refract

Dependent on elasticity and density of rock

Wave Speed

Crust/Mantle boundary - abrupt increase in P Wave speed

Moho

Abrupt decrease in wave speed

Core-Mantle Boundary

Secondary abrupt increase in wave speed

Outer-to-Inner Core Boundar

Created by S-wave inability to pass through core

Shadow Zone

Details variations in seismic velocity ofmaterials within the Earth

Seismic Tomography

Generated by motion in the liquid outer core, deflects solar wind

Magnetic Field