Science

continental drift

the hypothesis that a single large landmass broke up into smaller landmasses to form the continents, which then drifted to their present locations

mid-ocean ridge

a long, undersea mountain chain that has a steep, narrow valley at its center, forms as magma rises from the athenosphere, and that creates new oceanic lithosphere (sea floor) as tectonic plates move apart

sea-floor spreading

the process by which new oceanic lithosphere (sea floor) forms when magma rises to Earth's surface at mid-ocean ridges and solidifies, as older, existing sea floor moves away from the ridge

paleomagnetism

the study of the allignment of magnetic minerals in rock, specifically as it relates to the reversal of Earth's magnetic poles; also the magnetic properties that rock acquires during formation

plate tectonics

the theory that explains how large pieces of the lithosphere (plates) move and change shape

lithosphere

the solid, outer layer of Earth that consists of the crust and the rigid upper part of the mantle;

asthenosphere

the solid, plastic layer of the mantle beneath the lithosphere; made of mantle rock that flows very slowly, which allows tectonic plates to move on top of it

divergent boundary

the boundary between tectonic plates that are moving away from each other; dividing

transform boundary

the boundary between tectonic plates that are sliding past each other horizontally

convergent boundary

the boundary between tectonic plates that are colliding

rifting

the process by which Earth's crst breaks apart; can occur within continental crust or oceanic crust

terrane

a piece of lithosphere that has a unique geologic history and that may be part of a larger piece of lithosphere, such as a continent

supercontinent cycle

the process by which supercontinents form and break apart over millions of years

Pangea

the supercontinent that formed 300 milliion years ago and began to break up 200 milliion years ago

Panthalassa

the single, large ocean that covered Earth's surface during the time the supercontinent Pangea existed

deformation

the bending, tilting, and breaking of Earth's crust; the change in the shape of rock in response to stress

isostasy

a condition of gravitational and buoyant equilibrium between Earth's lithosphere and athenosphere

stress

the amount of force per unit are that acts on a rock

strain

any change in a rock's shape or volume caused by stress

fold

a form of ductile strain in which rock layer bend, usuallt as a result of compression

fault

a break in a body of rock along which one block slides relative to another; a form of brittle strain

mountain range

a series of mountains that are closely related in orientation, age, and model of formation

folded mountain

a mountain that forms when rock layers are squeezed together and uplifted

fault-block mountain

a mountain that forms where faulting breaks Earth's crust into large blocks, which causes some blocks to drop down relative to other blocks

dome mountain

a circular or elliptical, almost symmetrical elevation or structure in which the stratified rock slopes downward gently from the central point of folding

crust

the thin and solid outermost layer of the Earth above the mantle

mantle

the layer of rock between Earth's crust and core

core

the central part of the Earth below the mantle