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Unit 4 Vocab
Layers of the Earth and Plate Tectonics
Term | Definition |
---|---|
continental crust | thicker, less dense, older crust making the continents |
oceanic crust mantle | thinner, more dense, younger crust making ocean floor |
lithosphere | A rigid layer made up of the uppermost part of the mantle and the crust. |
asthenosphere | The soft layer of the mantle on which the lithosphere floats |
mantle | The layer of hot, solid material between Earth's crust and core. |
mesoshpere | the strong, lower part of the mantle between the asthenosphere and the outer core. |
outer core | A layer of molten iron and nickel that surrounds the inner core of Earth |
inner core | A dense sphere of solid iron and nickel at the center of Earth |
convection current | a current caused by the rising of heated fluid and sinking of cooled fluid; results in the movement of lithospheric plates |
lithospheric plates | the ratio of the mass of a substance to the volume of the substance (How tightly something is packed together) |
convergent boundary | A plate boundary where two plates move toward each other |
divergent boundary | A plate boundary where two plates move apart, resulting in upwelling of material from the mantle to create new seafloor. |
mid-ocean ridge | An underwater mountain chain where new ocean floor is formed |
transform boundary | A plate boundary where plates slide past each other |
subduction zone | the process by which one lithospheric plate moves beneath another as a result of tectonic forces |
plate tectonics | A theory stating that the earth's surface is broken into plates that move. |
fault | A crack in Earth's crust along which movement has occurred. |
continental drift | The hypothesis that states that the continents once formed a single landmass, broke up, and drifted to their present locations |
Pangea | A supercontinent containing all of Earth's land that existed about 225 million years ago. |