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27 Cards in this Set

  • Front
  • Back
continental drift
1912 alfred wegener stated that the continents move
pangae
wegener named the continents that formed the single landmass pangae which means all lands
panthalassa
surrounding pangae was the ocean which ment all seas
mesorsaurus
small extinct land reptile that live 270 million years ago which had been found in eastern south america and western africa
mid atlantic ridge
an undersea mountain range with a steep narrow valley running down the center that scientists mapped out in 1947
mid ocean ridges
65000 km long that goes around the earth
sea floor spreading
named after dietz, when the continents moved away from both sides of the ridge
plate tectonics
describes continental movement but also proposes a possible explanation of why and how continents move
tectonics
comes from greek word meaning tektonikos, which means construction, study of the formation of features in the earths crust
oceanic crust
material on the ocean floor
continental crust
makes up the continental landmass
lithosphere
made up by the oceanic and continental crust
asthenosphere
a later of plastic rock, it is solid but flows like "putty" when underpressure
divergent boundry
two plates that move away from eachother. found on the ocean floor. and they follow the mid ocean ridges
rift valley
center of the mid ocean ridge that is a narrow valley which forms as the plates separate.
convergent boundary
direct collision of one plate with another makes another type of plate boundry
subduction zone
refers to the place along a plate boundary where one plate moves under another plate
ocean trench
forms along a subduction zone.
subducted
forced under the less dense continental crust
island arc
part of the subducted plate melts and the molten rock rises to the surface along the trench to form a chain of volcanic islands
transfom fault boundary
two plates are grinding past eachother
convection
the transfer of heat through the movement of heated fluid material
convection current
the cycle of warm water rising and cool water sinking to replace it
theory of suspect terranes
suggests that continents are actually a patchwork of terranes which has its own distinct geological history.
terranes
pieces of lithosphere
1. contains rock and fossils that differ from neighboring terranes
2. major faults at the boundaries of terranes
3. magnetic properties of a terrane do not match those of neighboring terrans
normal polarity
magnetic minerals in newely formed rock orients towards magnetic north
reversed polarity
magnetic minerals in newly formed rock orient to magnetic south