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Science Plate Tecton

TermDefinition
mid-ocean ridges where youngest rocks on the seafloor are located; occur at divergent plate boundaries
lithosphere the Earth's crust and upper mantle
asthenosphere layer of the Earth on top of which the lithosphere floats
evidence of continental drift fossils, rocks, and magnetic reversals recorded in the seafloor
continental drift the hypothesis that continents have slowly moved to their current locations
divergent boundaries boundaries where plates move apart Example: the Great Rift Valley in Africa
Pangaea a single super-continent that once existed
transform boundaries boundaries where tectonic plates slide past each other Example: the San Andres Fault in the United States
convergent boundaries boundary between two plates moving together Example: the Himalayan mountain range in India
seafloor spreading opening in the seafloor that causes molten material beneath the Earth' s crust to rise to the surface
Glossopteris fossil plant that supports the theory of continental drift
magnetometer a sensitive device used to detect magnetic fields on the seafloor
convection currents currents inside the Earth that drive plate motion; the downward motion of a convection current causes tectonic plates to pull towards one another
Alfred Wegener proposed the theory of continental drift, but could not explain why or how the continents could move
ocean ridge vast, underwater mountain chain
mountain ranges form where two continental plates collide
subduction zone forms where two oceanic plates collide
uplift component of the rock cycle that brings metamorphic and igneous rock to the surface
subduction takes rock into the Earth where it will be melted
volcanic mountains a type of mountain formed when molten rock erupts onto Earth's surface and hardens
plateau area of relatively level high flat ground
Modified Mercalli Scale used to evaluate earthquake intensity based on the damage that results
earthquake when the force on rocks is great enough, they break, producing vibrations
epicenter the location on Earth's surface directly above an earthquake's focus; three seismographs are needed to accurately locate the epicenter
seismic waves energy that travels as vibrations on and in the Earth; help scientist discover changes in Earth's interior
reverse fault rock above the fault surface moves upward in relation to rock below the fault surface
strike-slip fault rock on either side of the fault surface move past each other
primary waves the first waves to reach a seismography after an earthquake occurs
focus the point in Earth's interior where the energy release of an earthquake occurs
Richter scale measures the magnitude of an earthquake
Created by: LOM8th
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