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Book F chapter 4

AB
continental driftcontinents have moved slowly to their current locations
Alfred Wegenerdeveloped the theory of continental drift
mesosaurusreptile fossil found in South America and Africa
glossopterisfossil plant found in Africa, Australia, and Antarctica
fossils of warm-weather plants found on this islandSpitzbergen, in the Arctic Ocean
Appalchian Mountains are similar to these rock structuresMountains in Greenland and Western Europe
seafloor spreadinghot, less dense material carries seafloor away from ridge
Harry Hessdeveloped the theory of seafloor spreading
Mid-ocean ridgesunderwater mountain ranges
sound waveshelped to discover mid-ocean ridges
This is how mid-ocean ridges are formedNew seafloor cools,contracts, becomes denser, and sinks
Found at the mid-ocean ridgesYoungest rocks in the ocean
Glomar Challenger had this toolDrilling rig to obtain rock samples from seafloor
Exotic life forms found on seafloorgiant clams, mussels, and tube worms
Magnetic reversals are recorded hereIron-bearing rocks formed in mid-ocean ridges
Magnetic time scaleProvided strong support that seafloor spreading was occurring
platessections of Earth's crust and upper mantle
plate tectonicsplates float & move around on the asthenosphere
lithosphereEarth's crust and part of upper mantle
asthenosphereplasticlike layer below lithosphere
divergent boundaryplates are moving apart
convergent boundaryplates move together
subductionoceanic plate sinks under continental plate
transform boundaryplates slide past one another
convection currentcycle of heating,rising,cooling,sinking
strike-slip faultrocks on opposite sides of a fault move in opposite directions or same direction but at different rates
Satellite Laser Ranging Systemmeasures movement of Earth's plates



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