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Earth’s Changing Structures
SSA Review 5 – Earth’s Changing Structures
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Earth’s Interior Layer Depth Temp Description Crust 3 – 25 miles
Solid rock, covered with land and oceans. Up to 230° F
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Earth’s Interior Layer Depth Temp Description Mantle
Goes down to 1,800 miles From 230° to 4400° F Made of rock material Lithosphere * top part ( miles) * solid rock * combines with the crust Asthenosphere * below the lithosphere * miles below the Earth’s surface *hot, melted rock (magma)
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Convection in the Earth’s Mantle
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Earth’s Interior Layer Depth Temp Description Core
Goes down to 3,900 miles 4,400 to 10,000°F Made of metal: nickel and iron. Outer core * 1,800-3,100 miles below Earth’s surface *liquid metal As hot as the sun Inner core *3, miles below Earth’s surface *solid ball of metal *very high pressure
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Mid-ocean Ridge – an underwater chain of mountains along the ocean floor.
*35,000 miles long
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Sea-floor spreading: at the mid-ocean ridge, magma rises from the mantle and erupts.
The lava spreads out, pushing older seafloor away from the ridge, adding new rock material to the ocean floor.
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Subduction - The process where the ocean floor sinks into a trench and down into the mantle.
Ocean trench - An underwater canyon that forms where the Oceanic crust sinks downward.
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Plate Boundaries – the cracks that separate the Earth’s tectonic plates
Juan de Fuca Plate Phillipine Plate Cocos Plate
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Types of Plate Boundaries
Name Description Two plates sliding past one another at a fault ( a crack in the Earth’s crust.) 1-Transform *Earthquakes occur along these boundaries.
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Rift valleys form at divergent boundaries on land.
Description Name 2 - Divergent Two plates moving apart from one another. *Divergent boundaries in the ocean occur at the mid-ocean ridge. (Sea-floor Spreading) Rift valleys form at divergent boundaries on land.
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Description Name 3 - Convergent
Two plates moving into one another. *Oceanic plates sink into a trench. Most volcanoes form here.
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Name Description Two plates moving into one another. Convergent *Mountains form when two continental plates collide and the land pushes upward.
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