A | B |
Pangaea | super continent that existed 200 million years ago |
Atlantic | ocean created when the super continent broke apart |
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 |
magnetic stripes | bands of ocean floor that show many magnetic reversals |
lithosphere | the crust and upper mantle |
mantle | the largest layer inside Earth |
crust | outermost layer of Earth |
inner core | solid core composed of dense iron and nickel |
outer core | liquid core composed of iron and nickel |
asthenosphere | plastic layer below the lithosphere that can flow |
plates | large sections of Earth's lithosphere |
plate tectonics | theory that Earth's lithosphere is broken into sections |
continental drift | theory that the continents move, and were once joined in a single landmass called Pangaea |
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 alongside each other |
convection current | cycle of heating, rising, cooling and sinking in fluids |
subduction zone | area where a denser converging plate sinks under a less dense converging plate |
San Andreas Fault | example of a transform fault boundary, found in California |
mid-ocean ridge | example of a divergent boundary in ocean crust |
Great Rift Valley in Africa | example of a divergent boundary in continental crust |
Marianas trench | deepest spot in any ocean, an example of converging oceanic plates |
Himalaya Mountains | example of a boundary where continental crust collided |
magnetic reversal | changes in Earth's magnetic field that result from movement in the outer core |
a few centimeters (an inch) | the average rate the plates move per year |
granite | the main type of rock found in continental crust |
basalt | the main type of rock found in oceanic crust |