Plate Tectonics and the Ocean Floor

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These flashcards cover key vocabulary and concepts related to plate tectonics and ocean floor geology for exam preparation.

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16 Terms

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Plate tectonics

A theory explaining the structure of the Earth's lithosphere, where tectonic plates move and cause geological phenomena.

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Continental drift

The theory that continents have moved over geological time and were once joined as a supercontinent.

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Pangea

The name of the supercontinent that existed around 335 million years ago, before breaking apart into the current continents.

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Glossopteris

A fossil fern with large seeds used as evidence for continental drift, found across southern hemisphere landmasses.

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Paleomagnetism

The study of the record of the Earth's magnetic field in rocks, used to support the theory of plate tectonics.

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Divergent boundary

A tectonic plate boundary where plates move away from each other, leading to the formation of new crust.

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Convergent boundary

A tectonic plate boundary where plates collide, leading to subduction or mountain formation.

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Transform boundary

A tectonic plate boundary where plates slide past one another horizontally, causing earthquakes.

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Slab pull

A force driving the movement of tectonic plates where the denser oceanic plate sinks into the mantle during subduction.

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Active margin

A coastal area where tectonic plates meet, characterized by high seismic activity and volcanism.

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Passive margin

A coastal area that is not a plate boundary, characterized by thick sediment deposits and minimal tectonic activity.

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Asthenosphere

The semi-fluid layer beneath the lithosphere that allows tectonic plates to move.

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Sea floor spreading

The process by which new oceanic crust is created at mid-ocean ridges as tectonic plates pull apart.

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Benioff zone

A plane of earthquakes that occur in a subduction zone, identified by the dipping pattern of the earthquakes.

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Fossil evidence

Remains or traces of ancient plants and animals used to infer past geological conditions and support continental drift.

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Continental crust

The layer of igneous, sedimentary, and metamorphic rocks that forms the continents, generally less dense than oceanic crust.