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Features of Plate Tectonics. Science 10. Layers of the Earth. Crust outer layer – thinner under oceans than under continents Broken into plates. Mantle T hickest layer – upper mantle is partly liquid– lower mantle is solid rock with Mg and Fe
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Features of Plate Tectonics Science 10
Layers of the Earth Crust • outer layer – thinner under oceans than under continents • Broken into plates
Mantle • Thickest layer – upper mantle is partly liquid– lower mantle is solid rock with Mg and Fe • Mantle convection occurs in liquid upper mantle
outer core – liquid Fe and Ni • inner core – solid Fe and Ni – 5000-6000oC
The crust and part of the upper mantle make up the lithosphere, which is broken into tectonic plates
The rest of the upper mantle is called the asthenosphere – this is where mantle convection occurs…. These currents are what cause the tectonic plates to move
Earth’s outer layer made up of separate, rigid slabs called plates • These plates move at speeds of between 2 cm and 10 cm per year -move due to “convection currents”
Push and Pull Ridge Push • As magma reaches the surface and cools, it pushes older material to the side
Slab pull • As a tectonic plate moves beneath a less dense plate (known as subduction), the plate pulls the rest of the plate with it
Plate Boundaries • Are regions where two plates interact • There are 3 main types
Divergent Boundaries • Plates move/pull away from each other • Example: Mid Atlantic Ridge • Features include Oceanic/Spreading Ridge (ocean) or Rift Valley (on land)
Convergent Boundaries • Plates move towards each other and collide. • 3 possible scenarios: • Oceanic-continental • Ocean-oceanic • Continental-continental
Oceanic-Continental Convergence • Oceanic plate slides beneath continental plate because it is oceanic is more dense • Features include: underwater valleys (trench) and volcanoes (volcanic belt) • Example location: West Coast of North America
Oceanic-Oceanic • Older, cooler oceanic plate will slide beneath other plate • Features include: volcanic island arc • Example locations: Japan, Indonesia, island of Alaska
Continental-Continental • 2 similar continental plates collide • Features: Large mountain ranges • Example locations: Himalayas
Transform Boundaries • Plates slide past each other • Features: Breaks in rock called faults and earthquakes • Example location: California’s San Andreas Fault