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Chapter 4: Cont. Drift, Sea-Floor Spreading, Plate Tectonics

AB
Alfred WegenerHe hypothesized that all the continents had once been joined into a supercontinent
PangaeaThe name of the supercontinent
Continental driftWegener's theory that the continents slowly move across the Earth's surface
MesosaurusA freshwater reptile that Wegener used as fossil evidence for continental drift
GlossopterisAn ancient plant found on widely separated continents. Provides evidence of continental drift.
Mid ocean ridgeThe underwater mountain chain where new sea floor is made.
SonarThis was used by Hess to make maps of the ocean floor.
Sea floor spreadingThe process by which molten material adds new oceanic crust to the ocean floor
Harry HessBuilt on Wegener's ideas and proposed the theory of sea-floor spreading
BasaltLava rocks that made up the mid-ocean ridge
Magnetic stripesPatterns in the sea floor that show reversals of the Earth's magnetic field; used as evidence for sea-floor spreading
Drilling samplesRocks taken from both sides of the mid-ocean ridge have the same age and pattern; the oldest ones are further from the ridge
trenchAn underwater canyon formed from subduction
SubductionThe process by which oceanic crust sinks back into the mantle
PlateA piece of the lithosphere that includes pieces of continental and oceanic crust
Ring of FireThe major earthquake and volcano zone located in the Pacific Ocean
Plate tectonicsThe theory that pieces of the Earth's lithosphere are in constant motion
Transform boundaryA plate boundary where two plates slide past each other in opposite directions
Convection currentsThese cause the Earth's plates to move
Divergent boundaryA plate boundary where two plates are spreading apart
Rift valleyA deep valley that forms where two plates move apart at a divergent boundary
Convergent boundaryA plate boundary where two plates are colliding
Andes MountainsA real world example of an oceanic-continental convergent boundary
JapanA real world example of an island arc
island arcThis is created at an oceanic-oceanic convergent boundary
HimalayasA real world example of a continental-continental convergent boundary
PacificThis ocean that is shrinking because there is so much subduction and very little sea-floor spreading
AtlanticThe ocean that is expanding because there is so little subduction and so much sea-floor spreading
SpitsbergenAn island near the north pole where Wegener found tropical plant fossils
Glacier scratchesMarks found in Africa, India, and Australia that indicated to Wegener that those places used to be cold!
Coal fieldsLand features used by Wegener that matched up in North America and Europe
J Tuzo WilsonThe scientist who put together the Theory of Plate Tectonics
San Andreas FaultA real world example of a transform boundary


6th grade science teacher
Aliso Viejo Middle School

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