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( OUTER CORE - liquid) ( INNER CORE - solid) metallic alloys magnetic, generates geomagnetic field dense, creates gravity nickel-iron alloy |
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( continental (granitic) - alumino-silicates, quartz, 10-100km, light) ( oceanic (basaltic) - alumino-silicates & silicates, 10-15km, dense) |
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(THICK - 2900km, iron and magnesium oxides and silicates, denser than crust) |
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Rgeological (Mechanical) Layers |
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- CRUST + OUTER MANTLE - 100km thick - rigid & strong - made of moving sheets & plates - plate tectonics - gets torn apart horizontally by loops due to convection (material form lower mantle rises) |
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- INNER MANTLE - below 100km - weak, soft, deform plastically or as highly viscous liquid putty - very little aluminum oxide & silicate minierals - MUCH DENSER - high pressure - lots of iron |
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heat rises from asthenosphere, circulating loops moving from melted areas (rising & sinking) |
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plates moving apart, basalt fills space between them |
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where plates move together |
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plates moving past one another in opposite directions - STRIKE-SLIP FAULTS (lots of earthquakes) |
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when slow-flowing, rising currents in the Earth's asthenosphere pull apart and TEAR A PREEXISTING PLATE INTO TWO OR MORE SMALLER PLATES |
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the process of plate growth at mid ocean ridges from erupting expanding molten material throughout the period of divergence |
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When two converging plates meet - the denser of the two plates dives beneath the other and sinks into the Earth's interior where it is consumed
Oceanic plates are denser than continental - always will dive when meeting a continental plate
Metamorphic rock formed where plates meet as rocks of higher plate are deformed |
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when two continental plates come together neither is dense enough to subduct to the denser material below - plates weld together instead of subducting, forming a larger single plate - forming mountain ranges at border of plates |
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