Tectonics: 1.4 - Earth's Conveyer Belt Flashcards
Earth’s structure
Inner core: solid steel
Outer core: 2,300 km of molten liquid metal -> flows because of Earth’s rotation -> creating a magnetic due to metal in outer core -> but it’s unstable so polarity swaps every 200,000 years
Mantle: peridotite (rock with high concentration of magnesium, and also iron and silica)
Crust: igneous, metamorphic and sedimentary rock
Lithosphere
Crust and upper mantle
Asthenosphere
Layer of mantle below lithosphere
90% of heat at depth comes from…
Radioactive decay, as well as some latent heat from core
Decompression melting
As the pressure decreases the melting point of substances decreases
This means rock in the mantle melts as it rises, creating magma
This is why the asthenosphere acts like soft toffee
Mid-ocean Ridge
Formed when magma collects in chambers, rises to the surface, and cools
This buildup of material creates a ridge
Sea floor spreading
Combination of ridge push and slab pull
Ridge push
When a ridge collapses under its own weight, pushing tectonics plates away
Slab pull
When a tectonic plate subducts into the mantle under its own weight, pulling the whole plate down
Palaeomagnetism
Lava on surface contains magnetic material. When lava cools these materials align with the Earth’s North and South Poles at the time
Ridge push causes materials to split, both facing ‘North’. When polarity swaps, materials align with the new ‘North’ (old South), facing the opposite direction. Ridge push causes material to split, etc.
Evidence for sea floor spreading
Palaeomagnetism