internal formation of earth Flashcards
crust - properties
less than 1% of earth’s mass
broken rock
2.7 kg/cm3 density
oceanic crust and continental curst depth difference
oceanic - 5-10km
continental - 30-70km avg (35km)
oceanic crust and continental crust density difference
oceanic - 3 kg/cm3
continental - 2.6-2.7 kg/cm3
oceanic crust and continental crust mineral composition difference
oceanic - basaltic, silicon and magnesium
continental - granitic, silicon and aluminium
mantle - properties
70% of earth’s mass
plastic state
depth 30-3030 km
density 3.5-5.5 kg/cm3
core - properties
30% of earth’s mass
semi-liquid state
depth 3030 - 6370 km
density 10-12 kg/cm3
mantle
The mantle layer is the largest layer of the earth
molten silicates and minerals
source of earths inner heat = convection currents
thickness of around 2886 km
70% of the mass of earth
crust
surface of the earth
lithosphere
fragile external shell of Earth, including the crust and upper mantle layer.
Asthenosphere
a thick layer of plastic upper mantle
location of strong tectonic forces = natural events
outer core
iron and nickel
liquid - because of less pressure and high temperature
inner core
iron and nickel
solid - because of high temperature and high pressure
mohorovičič / Moho Discontinuity
the junction between then earth’s crust and the mantel where seismic waves are modified