A | B |
Pangaea | super continent that existed 200 million years ago |
Alfred Wegener | scientist who thought that the continents were once one super continent |
sea-floor spreading | theory that new ocean crust is formed at the mid ocean ridges by molten lava |
lithosphere | crust and upper mantle |
mantle | the largest layer inside Earth |
crust | outer most layer of Earth |
inner core | solid core composed of dense iron and nickel |
outer core | liquid core composed of iron and nickel |
plates | large sections of Earth's crust and upper mantle, lithosphere |
plate tectonics | theory that Earth's crust and upper mantle are broken into sections |
continental drift | theory that the continents move |
divergent boundary | boundary between two plates that are moving apart |
convergent boundary | boundary where two plates are moving toward each other |
transform fault boundary | boundary where two plates are moving past each other |
convection current | cycle of heating, rising, cooling and sinking |
mid-ocean ridge | example of a divergent boundary in ocean crust |
conduction | The transfer of heat by direct contact. |
convection | Heat transfer by the movement of currents through liquid. |
radiation | Transfer of heat through empty space. |
convergent boundary | Point where two plates collide with each other. |
granite | Rock continental crust is made of. |
basalt | Rock oceanic crust is made up of. |
mountain | Formed as a result of two continental plates converging. |