tectonics Flashcards
who proposed the idea of continental drift
Alfred Wegener, 1912 Pangaea
- Asserted Pangaea had broken into pieces were still moving apart - related to the spinning Earth
what is density
mass per unit volume
what is the density stratification like on earth
denser substances towards the center
what kind of waves do earthquakes generate
seismic waves
2 types of seismic waves
surface waves - travel along Earth’s surface
body waves - travel through Earth
2 types of body waves
- P wave - compressional wave – refracted at density boundaries (travel 2x as fast as S waves in solids )
- S wave – shear wave – cannot pass through liquids
what is used to detect and record arrival times and intensity of seismic waves
seismograph
what did Oldham discover
“shadow zones” - different waves bend different ways in dense and less dense zones – able to get an idea of planet structure
crust characteristics
Earth’s rocky shell ~ 2-75 miles
- form shifting slabs of rock called tectonic plates
2 types of crust
Oceanic – basalt
Continental – granite
upper mantle characteristics
~400 miles thick
- The rigid top ~40 miles
lower mantle characteristics
~ 1400 miles thick
- extends to core – similar composition to asthenosphere, but does not melt due to rapid pressure increase – increases melting point
mantle characteristics
Oxygen, iron, magnesium, silicon - ~68% of Earth’s mass, 83% of volume
outer core characteristics
~1,400 miles thick
- Mostly iron and nickel
inner core characteristics
~ 1,500 miles in diameter
- Mostly iron
what factors determine the behaviour of the rock
temperature, pressure, rate at which stress is applied
Lithosphere characteristics
~ 44-125 miles depth
- crust + uppermost cool and rigid portion of mantle
- floats on (and is supported by) the denser deformable asthenosphere
Asthenosphere characteristics
~ 400 miles depth
- hot, partially melted, slowly flowing
upper core characteristics
dense, viscous liquid
inner core characteritics
solid, ~6 times denser than crust
what is earths internal heat maintained by
radioactive decay
- Heat transfer occurs via conduction (solid materials) + convection (fluids like the mantle)
what is buoyancy
Things sink until the same proportion of their volume is submerged – continents do this
what is Isostatic equilibrium
erosion of a top of a mountain causes their roots to rise to get equilibrium – cause continental crust to get thinner
crustal rock vs asthenosphere differences
- crustal rock = rigid and does not flow at surface temperatures
- Ships adjust to weight changes via buoyancy, but crustal rock cannot