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chapter 8 L1-L4

QuestionAnswer
The equilibrium between continental crust and the denser mantle below it. Isostasy
The downward vertical motion of Earth's surface Subsidence
The upward motion of Earth's surface Uplift
Squeezing stress Compression
Stress that pulls something apart Tension
Parallel forces acting in opposite directions Shear
A change in the shape of rock caused by stress Strain
Are deep, underwater troughs created by an oceanic plate subducting under another plate at a convergent plate boundary Ocean Trench
A curved line of volcanoes that form parallel to a plate boundary Volcanic Arc
Where block of crust slide horizontally past each other Transform Fault
An area of many fractured pieces of crust along a large fault Fault Zone
are made of layers of rocks that are folded Folded Mountain
are parallel ridges that form where blocks of crust move up or down along the faults Fault-block Mountain
An extensive area of level or rolling land Plains
Areas of subsidence and regions with low elevation Basin
Flat regions with high elevations. Plateau
When large regions rise vertically with very little deformation. Uplifted Mountain
Created by: cassius s-c
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