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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 |