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A set of vocabulary flashcards covering plate tectonics, physical and chemical weathering processes, and mass movements based on the lecture materials.
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Lithosphere
The upper surface layer of the Earth, including the crust and the upper mantle, which is about 70km deep.
Continental crust
A layer of the Earth’s crust that is 35–70km thick on average, very old, and primarily granitic in nature.
Oceanic crust
A layer of the Earth’s crust that is 6–10km thick on average, very young, and primarily basaltic in nature.
Convection current theory
A theory stating that huge currents occur in the Earth's interior where magma rises due to radioactive decay and spreads at mid-ocean ridges.
Hotspot
A plume of lava that rises vertically through the mantle, such as the Hawaiian hotspot, which may create a drag force causing plate movement.
Paleomagnetism
The phenomenon where magnetic grains in cooling lava acquire the direction of the Earth's magnetic field at the time of cooling.
Sea-floor spreading
A process occurring at constructive margins where ocean floors grow and new oceanic crust is created as plates move apart.
Subduction
The process where one plate is forced downwards into the mantle at a convergent boundary, often forming deep-sea trenches.
Transform fault
A fault zone created where plates slide past one another without colliding or separating, often associated with shallow earthquakes.
Ocean ridges
Giant submarine mountain chains with a total length of more than 60,000km that rise 2–3km above the surrounding ocean basins.
Island arcs
A volcanic island chain formed in an arc-shape when oceanic lithosphere is subducted beneath other oceanic lithosphere.
Weathering
The decomposition and disintegration of rocks in situ.
Freeze–thaw
A physical weathering process where water in cracks freezes at 0∘C, expanding by about 10% and exerting pressure up to 2100kg/cm2.
Exfoliation
A physical weathering process in hot deserts where the outer layers of rock peel due to stresses from a large diurnal temperature range.
Salt crystallisation
The decomposition of rock by salt solutions, where substances like Na2SO4 and Na2CO3 expand by about 300% between 26–28∘C.
Pressure release
The process whereby underlying rocks expand and fracture parallel to the surface after overlying rocks or weight are removed by erosion.
Hydrolysis
A chemical weathering process where minerals like orthoclase feldspar in granite react with acidic water to form kaolin or china clay.
Hydration
A process where certain minerals absorb water and expand, such as when anhydrite is changed into gypsum.
Carbonation–solution
A chemical process where weak carbonic acid formed from rainfall and CO2 reacts with calcium carbonate to form soluble calcium bicarbonate.
Oxidation
A chemical reaction where iron compounds react with oxygen to produce a reddish brown coating, changing FeO to Fe2O3.
Chelation
The process in which plant roots absorb relatively insoluble minerals by exchanging hydrogen ions with cations in adjacent minerals.
Van’t Hoff’s law
The principle stating that the rate of chemical weathering increases 2–3 times for every 10∘C increase in temperature.
Tor
An isolated mass of bare rock, often granite, left standing on a hilltop after the surrounding rock has been broken down and removed.
Equifinality
A concept in geomorphology stating that different processes can produce the same end result.
Swallow holes
Depressions or sinks in the ocean floor or limestone surfaces, ranging from small-scale to large dolines up to 30m in diameter.
Regolith
The superficial and unconsolidated material found at the Earth’s surface, including soil, scree, and weathered bedrock.
Mass movements
Large-scale movements of the Earth’s surface that are not accompanied by a moving agent such as a river, glacier or ocean wave.
Shear strength
The internal resistance of a slope to mass movement.
Shear stress
The forces attempting to pull a mass downslope.
Tailings
The impurities left behind after a mineral has been extracted from its ore during the mining process.