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continental drift
the theory suggesting that the Earth’s crust is split up into large slabs called plates that slowly move along the Earth’s surface
plate tectonics
the theory suggesting that the Earth’s crust is split up into large slabs of solid rock called tectonic plates
Gondwanaland
the ancient supercontinent of the southern hemisphere
Pangaea
the supercontinent from around 300 million years ago
Mesosaurus
an extinct freshwater reptile
Glossopteris
a seed fern
magnetic anomalies
a stripy pattern in plates because of a variation in the Earth’s magnetic field/the reversal of the Earth’s poles
Benioff zone
a zone of earthquakes close to ocean trenches
outer core
a fluid layer of the Earth composed of mostly iron and nickel
inner core
the innermost layer of the Earth that is about 2414km thick
mantle
the mostly solid layer of the Earth between the core and the crust that is about 2900km thick
asthenosphere
the zone of the Earth’s mantle between the lithosphere that is hot and fluid
lithosphere
the rigid layer of the Earth made up of the crust and the solid outermost layer of the upper mantle
Moho (Mohorovicic discontinuity)
the boundary between the crust and the mantle of the Earth
crust
the outermost shell/layer of the planet
mid-ocean ridges
seafloor mountain systems
subduction zone
where oceanic crust sinks back into the mantle
viscosity
the resistance of a fluid to change shape/the thickness of a fluid
slab pull
the force that is generated from denser oceanic plates subducting beneath less dense continental plates at subduction zones
mantle plumes
a mechanism of convection within the Earth’s mantle