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Earth Dynamics

AB
compressionstress resulting from squeezing
isostasyequilibrium between continental crust and the denser mantle below it
shearstress resulting from parallel forces acting in opposite directions
strainchange in the shape of rock caused by stress
subsidencedownward vertical motion of Earth?s surface
tensionstress that pulls something apart
upliftupward vertical motion of Earth's surface
fault zonearea of many fractured pieces of crust along a large fault
ocean trenchdeep, underwater trough created by one plate subducting under another plate at a convergent plate boundary
transform faultarea where tectonic plates slide horizontally past each other
volcanic arccurved line of volcanic islands that forms parallel to a plate boundary
fault-block mountainparallel ridges that form where blocks of crust move up at faults
folded mountainmade of layers of rocks that are folded
uplifted mountainforms when large regions rise vertically with very little deformation
basinarea of subsidence and region with low elevation
plainsextensive areas of level or rolling land
plateauflat region with high elevation


Science Teacher 6th and 7th Grade
Raa Middle School
Tallahassee, FL

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