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Chapter 8

QuestionAnswer
Isostasty equilibrium between continental and the denser mantle below it.
subsidence the downward vertical motion of earth's surface
uplift upward vertical motion of earth's surface
tension stress that pulls something apart
compression squeezing stress
strain change in the shape of rocks caused by rocks
ocean trenches are deep underwater troughs created by an oceanic plate
volcanic arc curved line of volcanoes that forms parallel to a plate boundary
transforms fault blocks of crust slide horizontally past each other
fault zone area of many fractured pieces of crust along a large fault
Folded mountains made of layers of rocks that are folded
Fault-block mountains parallel ridges that form where blocks pf crust move up or down along faults
plain extensive area of level or rolling land
basins area of subsidence and regions with low elevation
plateaus flat regions with high elevations
Created by: Lorena R.
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