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25 Cards in this Set

  • Front
  • Back
Continental drift
1912-- Alfred Wegener-- hypothesis that stated that the continents had moved.
Pangaea
single landmass thought to have been the origin of all continents.
Panthalassa
giant ocean surrounding Pangaea.
Mesosaurus
a small extinct land reptile that lived 270 million years ago.
Mid-Atlantic Ridge
undersea mountain range with a steep, narrow valley along its center.
mid-ocean ridges
system of undersea mountain ranges that wind around the earth.
seafloor spreading
movement of the ocean floor away from either side of a mid-ocean ridge.
plate tectonics
theory that the lithosphere is made up of plates that float on the asthenosphere and that the plates possibly are moved by convection currents.
tectonics
comes from the Greek word tektonikos , meaning "construction". Tectonics is the study of the formation of features in the earth's crust.
oceanic crust
material that makes up the ocean floor.
continental crust
material that makes up landmasses
lithosphere
thin outer shell of the earth consisting of the crust and the rigid upper mantle.
asthenosphere
zone of mantle beneath the lithosphere that consists of slowly flowing solid rock.
divergent boundary
boundary formed by two lithospheric plates that are moving apart.
rift valley
steep, narrow valley formed as lithospheric plates separate.
convergent boundary
border formed by the direct collision of two lithospheric plates.
subducted
forced.
subduction zone
region where one lithospheric plate moves under another.
ocean trench
deep valley in the ocean floor that forms along a subduction zone.
island arc
chain of volcanic islands formed along an ocean trench.
transform fault boundary
boundary formed where two lithospheric plates slide past each other.
convection
transfer of heat through the movement of a fluid material.
convection current
movement in a fluid caused by uneven heating.
theory of suspect terranes
theory that continents are a patchwork of pieces of land that have individual geologic histories.
terranes
piece of land with a geologic history distinct from that of the surrounding land.