Plate Tectonics Review

About this set

Created by:

rbartlett  on October 16, 2008

Description:

A review set for the Earth Science Plate Tectonics Unit.

Classes:

Honors Earth and Environmental Science, Earth and Environmental Science, OGBiology, Self Contained Biology, Earth Science

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Plate Tectonics Review

Theory of Continental Drift
Theory that continents move due to centrifical force
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Theory of Continental Drift Theory that continents move due to centrifical force
Theory of Plate Tectonics Theory that plates that move due to convection currents
Alfred Wegener credited with the theory of Continental Drift
Harry Hess credited with the theory of Plate Tectonics
sea floor spreading when two oceanic plates pull apart, magma rises and new crust is formed
convection currents circular movement of a substance due to changes in temperature and density
plates large pieces of earths crust that move due to convection currents
oceanic crust earths crust located under the ocean
continental crust earths crust made of land
pangea large supercontinent that existed 250 million years ago
divergent boundary when two plates pull apart
convergent boundary when two plates come together
transform boundary when two plates grind past each other
rift valley formed when two plates pull apart and land falls downard
island arc a chain of volcanic islands formed at an ocean-ocean convergent boundary
volcanic arc a chain of volcanic mountains formed at an ocean-continental convergent boundary
mountain range formed at a continental-continental convergent boundary
subduction zone the more dense plate us pulled into the mantle under the less dense plate
Mid Atlantic Ridge divergent boundary in the middle of the Atlantic Ocean
trench depression formed at a subduction zone
lithosphere another name for the crust
aesthenosphere another name for them mantle
crust outer layer of the Earth, the thinnest layer
mantle thickest layer of the Earth, part liquid part solid where convection currents are found
mountain range form at continental-continental convergent boundaries
temperature inside Earth increases with depth
pressure inside Earth increases with depth
fault a break in the earths crust that moves
igneous rock formed from cooling lava
hot spot area where magma from the mantle continually breaks through the crust
hot spot example Hawaiian islands
age of ocean rocks younger near sea floor spreading zone
high risk cities cities where earthquakes and volcanoes are likely to happen
low risk cities cities where earthquakes and volcanoes are not likely to happen
plate tectonics evidence rocks, fossils, climate, puzzle fit, glaciers, sea floor spreading
rate of plate movement 5 cm/year
rock crystals form when rocks cool slowly
crust density ocean crust is more dense
Wegener's evidence fossils, rocks, climate
Wegener's flaws how continents moved

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