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Many metamorphic rocks contain large and beautiful crystals. The diverse
colors and textures of these rocks resulted from different combinations
of temperature and pressure produced by interactions of the gigantic
tectonic plates that cover Earths surface. The rocks formed either where
one plate sank below another (subduction zone) or where two plates
collided. |
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![[Diagram: Various rocks pictured in a diagram explaining where they typically form.]](images/3_0_0_0/3_2_4_2_main.jpg)

Two geothermstemperature/pressure
curvesshow how these parameters increase as you go deeper into
the Earth. One is for subduction zones, the other for collision
zones. |