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 |
Mesosaurus | reptile fossil found in South America and in Africa |
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 |
asthenosphere | plastic layer below the lithosphere |
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 |
subduction zone | area where a denser converging plate desends or sinks under a less dense converging plate |
San Andreas Fault | example of a transform fault boundary |
mid-ocean ridge | example of a divergent boundary in ocean crust |
Himalaya Mountains | example of boundary where continental crust collided |
constructive force | force that builds up the Earth's surface |
destructive force | force that breaks down Earth's surface |
Geologist | scientist who studies the forces that make and shape Earth |
basalt | cooled lava rack, makes up oceanic crust |
granite | light rock, makes up continents |
theory | an idea that has not yet been proven false |