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Earth Science: Unit 4 Chapter 10

Plate Techtonics, Earth Quakes

AB
Alfred Wegenerproposed theory of continental drift
continental drifthypothesis that continents were once a single landmass that broke up and drifted apart
fossil evidenceidentical fossils on different continents to prove continental drift theory
rock formation evidencematchin rocks on different continents to prove continental drift theory
climatic evidenceevidence to prove continental drift theory shoing glaciers in various locations
continents plowed through ocean basinWegener's theory that had no basis
mid-ocean ridgeslong, undersea mountain chains formed from magma under ocean
sea-floor spreadingprocess where new ocean floor is created as magma rises and solidifies
paleomagnetismstudy of magnetic alignment of mineral in rocks relating to earth's magnetic poles
continental plateplate with a continent on it; contains part oceanic crust too
oceanic plateplate containing only oceanic crust
evidence for plate techtonics part 1mid-ocean ridges;earthquake/volcano patterns; shapes of continents
evidence for plate tectonics part 2age of sea floor;patterns of magnetic reversals;heat from interior greatest along ridge
evidence for plate tectonics part 3fossil evidence;similiar rock and mountain ranges
lithospheresolid, outer layer of Earth containing crust and rigid upper mantle
aesthenospheresolid, plastic layer of mantle beneath lithosphere;slow moving liquid rock
techtonic platelarge pieces of lithosphere that are believed to move and change shape
divergent boundaryboundary between tectonic plates moving away from each other
convergent boundaryboundary between tectonic plates that are colliding
transform boundaryboundary between tectonic plates that are sliding past each other horizontally
events occurring at plate boundariesearthquakes and volcanoes
2 features where plates move apartmid-ocean ridge and rift valley
does not produce magmatransform boundary
causes of plate motionconvection currents
convection currentsmovement of heated material due to differences in density caused by differences in temperature
ridge pushforce at mid-ocean ridge where sinking lithosphere causes plate to move away
slab pullplates pull away from each other at mid-ocean ridges forming new lithosphere
riftingprocess where Earth's crust breaks apart; continental or oceanic
terranepiece of lithosphere with unique geologic history
supercontinent cycleprocess where large landmasses formed and broke apart over millions of years
Pangeasupercontinent formed 300 million years ago that began breaking up 250 million years ago
cratonslarge areas of stable rocks; older than 540 million years
shieldsrocks within cratons exposed at Earth's surface
effects of contintental change (moving continents)changes in climate and changes in life forms
ocean fromed as American continent separated from Europe and AfricaAtlantic Ocean


7th Grade Co-Teacher/Special Education & Yearbook Advisor
Caledonia-Mumford Middle School
Caledonia, NY

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