STRUCTURE OF THE EARTH Flashcards
earth layers
inner core, outer core, mantel (mesosphere, asthenosphere, lithosphere) , crust
inner core
solid
iron and nickel
outer core
iron, nickel and sulphur
* Liquid
* Magnetic field generation
o The liquid converts thermal and gravitational energy to magnetic energy creating the magnetic field
* Polar wandering
o Pole changes over time
* Magnetic north south reversal
o Not regular, have changed hundreds of times over 250 Ma
o Mantel
(less dense than core, Fe and Mg + silicate minerals (Si + O), silicate minerals), mafic rocks, low temp gradient = convection
lower mantel
mesosphere
rigid
Asthenosphere
- Plastic
- At melting point
Uppermost mantel
Lithosphere)
* Rigid, floats on the asthenosphere
* Made of the upper mantel and crust
* Diamonds
crust
Oceanic or continental
Granitic and basaltic)
Felsic rocks
temp and pressure profiles
Increase as they go inwards
Pressure is linear, temp is not
body waves
primary - compression
secondary - shear, cannot travel through liquid
seismology
o Study of vibration and waves within the earth
o Waves travel faster in stronger, dense materials
waves effected by
rock density
phase of rock (solid/liquid)
o Velocity increase with depth, boundaries marked by dramatic velocity changes and refraction of waves
Greater velocity is more angled line
Steeper line = less velocity
o Mohorovivic discontinuity
crust mantle boundary)
Waves reaching at different times after earthquakes, the denser material is faster = greater distance
CMB
core mantel boundary
S waves cannot travel through liquid
How we know outer core is liquid