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Earth's Structure C3
Continental drift, mid-ocean ridges, subduction, plate tectonics
Term | Definition |
---|---|
Alfred Wegener | German scientist that created the theory of continental drift |
Continental drift | Wegener's idea that the continents slowly moved over Earth's surface over millions of years |
Pangaea | Wegener's name for the supercontinent |
Fossil | Any trace of an ancient organism |
Glossopteris | A fernlike plant that lived 250 years ago whose fossils have been found in Africa, South America, Australia, India and Antarctica |
Mesosaurus, Lystrosaurus | Freshwater reptiles whose fossils have been found in places now separated by oceans, supporting the theory of continental drift |
Mid-ocean ridges | Long chains of mountains that rise up from the ocean floor |
Sonar | A device that uses sound waves to measure the distance to an object |
Sea-floor spreading | The process that continually adds new material to the ocean floor |
Deep-ocean trenches | Underwater canyons that the old ocean floor sinks into during subduction |
Subduction | The process by which the ocean floor sinks beneath a deep- ocean trench and back into the mantle again |
Divergent boundary | A boundary where plates diverge, or move away from each other |
Convergent boundary | A boundary where plates converge, or come together |
Transform boundary | A boundary where plates slip past each other |
Plate tectonics | A theory that states that Earth's plates are in a slow, constant motion, driven by convection currents in the mantle |
Plates | Pieces of the Earth that make up the lithosphere and are separated by cracks |
Faults | Breaks in Earth's crust where rocks have slipped past each other |
Rift Valley | A deep valley on Earth formed when plates diverge on land |