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convergent plate boundary: oceanic to continental plate

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convergent plate boundary: oceanic to continental plate

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the more dense oceanic plate sinks beneath the less dense, continental plate

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divergent plate boundary: continental to continental

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divergent plate boundary: continental to continental

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a continental plate spreads in two different directions, collapsing the central rift

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divergent plate boundary: oceanic to oceanic plate

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divergent plate boundary: oceanic to oceanic plate

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- oceanic plates move apart, new magma rises from the mantle to fill in the gap

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a plate boundary where 2 plates move away from each othe

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Harry Hess was a scientist that helped discover the process of sea-floor spreading.

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Alfred Wegener was a German Scientist who originally started off as a meteorologist. During his work he noticed the puzzle-piece, like shape of the continents, which eventually led to him proposing his theory of Continental Drift.

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when continental glaciers cover an area of land, they leave behind deeply carved grooves and scratches in the landscape and rock beds which they once covered. This is caused by the rocks/boulders that the ice sheets pick up and carry with them as they move over the land.

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a deep valley that forms where 2 plates move apart

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a section of the lithosphere that slowly moves over the asthenosphere, carrying pieces of continental and oceanic crust

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a plate boundary where 2 plates move towards each other

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a plate boundary where 2 plates move past each other in opposite directions

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a break in Earth's crust where slabs of rock slip past each other

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the movement of fluid, caused by differences in temperature, that transfers heat from one part of the fluid to another

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the theory that pieces of Earth's lithosphere are in constant motion, driven by convection currents in the mantle

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a well-tested concept that explains a wide range of observations

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the process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle (convergent boundary)

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a deep valley along the ocean floor through which oceanic crust slowly sinks towards the mantle

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the process by which molten material adds new oceanic crust to the ocean floor

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the undersea mountain chain where new ocean floor is produced (divergent boundary)

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the hypothesis the continents slowly move across Earth's surface