The rock on the left was the sedimentary rock shale. Now it's the metamorphic rock slate. Slate looks very similar to shale, but harder and more platy. The rock on the right is gneiss. The light and dark minerals have separated into bands. Gneiss is produced by higher temperature metamorphism. The original rock was different in both cases.
Common Metamorphic Rocks
Some of the most common metamorphic rocks are listed below (Table below). Their parent rock and the type of metamorphism are also mentioned.
The table shows some common metamorphic rocks and their original parent rock.
Picture
Rock Name
Type of Metamorphic Rock
CommentsSlate
Foliated
Metamorphism of shalePhyllite
Foliated
Metamorphism of slate, but under greater heat and pressure than slateSchist
Foliated
Often derived from metamorphism of claystone or shale; metamorphosed under more heat and pressure than phylliteGneiss
Foliated
Non-foliated
Contact metamorphism of various different rock typesQuartzite
Non-foliated
Metamorphism of quartz sandstoneMarble
Non-foliated
Metamorphism of limestoneMetaconglomerate
Non-foliated
Metamorphism of conglomerate
Summary
Foliated metamorphic rocks are platy.
Non-foliated metamorphic rocks are massive.
The more extreme the amount of metamorphism, the more difficult it is to tell what the original rock was.
Marble is metamorphosed limestone.
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