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Created by michelle danko
over 5 years ago
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Question | Answer |
layers of the earth | |
oceanic- thinner, less dense, basalt Continental- thicker, more dense, granite | |
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Th (binary/octet-stream)
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Lithosphere made up of crust and upper mantle |
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Moho (binary/octet-stream)
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MOHO between crust and rigid mantle |
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Esrt (binary/octet-stream)
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Most common elements in crust |
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Mantle (binary/octet-stream)
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thickest layer, part solid, part liquid |
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Asth (binary/octet-stream)
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Plastic mantle layer in which convention occurs |
convection currents in the asthenosphere move the plates around | |
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Core (binary/octet-stream)
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Believed to be entirely liquid iron and nickel. Evidence is that S waves do not pass through this layer |
inner core solid iron and nickle highest density | |
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Esrt10 (binary/octet-stream)
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properties of earth's interior |
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Graph (binary/octet-stream)
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temperature and pressure increase as you travel deeper into the earth |
The lithosphere of the earth is broken up into plates which “float” on the plastic asthenosphere below | |
Theory developed in the mid-1900’s that explained all geologic observations including mountains, earth- quakes, volcanoes, and trenches | |
convergent move towards each other | |
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Diver (binary/octet-stream)
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Divergent move away from each other forms a ridge |
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Trans (binary/octet-stream)
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Transform slide past one another earthquakes found here |
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Subd (binary/octet-stream)
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Subduction zone (continental crust and oceanic crust) The oceanic crust beneath because it is more dense Volcanoes, mountains, earthquakes and trenches |
HOT SPOTS • There are locations on earth, away from plate boundaries, where volcanic activity occurs | |
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Fold (binary/octet-stream)
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fold |
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Faults (binary/octet-stream)
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fault |
Collision zone (continental crust and continental crust) colliding plates with same density crumple up as they collide • Mountains and earthquakes | |
Island Arc (oceanic crust and oceanic crust) two oceanic plates collide and one usually subducts Volcanic islands, earthquakes and trenches |
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