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Tectonics Assessment

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Term
Definition
lithosphere   the outermost part of the Earth including the crust and upper mantle  
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convergent   two plates move towards each other, continental vs continental plates produce Fold Mountains eg. the Himalayas. Where oceanic vs continental plates, Subduction Zones are formed  
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divergent   two plates move away from each other, continental vs continental plates produce Rift Valleys eg. East African Rift Valley. Where oceanic vs oceanic plates Oceanic Ridges form eg. Mid-Atlantic Ridge.  
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subduction   oceanic vs continental plates move towards each other, due to the difference in density, the more dense oceanic plate sinks and is forced beneath the less dense continental plate  
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transform   two plates slide past one another, typically with a stick-slip motion - this produces seismic activity and earthquakes  
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asthenosphere   the ductile part of the earth just below the lithosphere, including the upper mantle  
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igneous   rocks such as Granite (below the surface) and Basalt (on the surface) formed from cooled magma  
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sedimentary   rocks formed by the deposition of layers of eroded 'sediments' under various conditions eg. Limestone, Sandstone and Shale  
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metamorphic   sedimentary or igneous rocks altered under intense heat or pressure eg. Marble and Slate  
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continental   plates are between 20-80 km thick and relatively less dense  
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oceanic   plates are thinner, around 10 km thick and relatively dense  
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hotspots   These are super heated areas of magma within the mantle which cause magma to break through the crust eg. Hawaiian Islands in the middle of the Pacific plate.  
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shield   found at constructive, divergent margins, produced by flows of fluid lava which forms gently sloping, low profile cones  
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composite   found at destructive, convergent margins, produced by layers of viscous lava and ash which form steep sloped, tall cones  
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cinder   found close to subduction zones, these are simply produced by layer upon layer of cooled 'blobs' or lava to form a circular or oval cone  
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fold   can be defined as a bend in rock that is the response to compressional forces  
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fault   can be defined as the displacement of once connected blocks of rock along a fault plane  
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epicentre   the point on the Earth surface directly above the focus  
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focus   There is a sudden movement within the crust or mantle, and concentric shock waves move out from that point  
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p-waves   They are high frequency, short-wavelength, longitudinal waves which can pass through both solids and liquids. The ground is forced to move forwards and backwards as it is compressed and decompressed.  
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s-waves   They move in all directions away from their source, at speeds which depend upon the density of the rocks through which they are moving. They cannot move through liquids  
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l-waves   similar to that of waves in the sea. The ground is made to move in a circular motion, causing it to rise and fall as visible waves move across the ground  
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tsunami   giant waves which result from underwater earthquakes or landslides  
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lahar   mudflow made up of volcanic debris  
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pyroclastic flow   super heated explosion of gas, ash and rock  
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lava flow   river of molten rock  
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