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Rocks > Non-Foliated Metamorphic Rocks
Non-foliated metamorphic
rocks are commonly transformed from their
parent rocks when they are touched by magma.
Characteristics
These rocks are characterized by a high density and hardness. Often
they have swirls of color, due to impurities being excluded from recrystallization.
How they are
formed
These rocks are recrystallized from single-mineral sedimentary
rocks, usually by being touched by very hot magma. Because the minerals
in their parent rocks are not flat like those in the parents of foliated
metamorphic rocks, they do not develop any flakes. When they are recrystallized,
any impurities in the rock are excluded, often creating swirls of color.
Where they are
found
These rocks can be found near where their parent rocks once were. Some
famous non-foliated metamorphic rocks include marble, which is formed
from limestone, and quartzite, which is formed from quartz sandstone.
Click
here to view Foliated Rocks
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Webmasters: Chris
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This page was last updated on December 4, 2000
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