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Metamorphic Rocks FORMED BY HEAT AND PRESSURE
OLDER ROCKS MAY BE FORMED INTO A NEW TYPE OF METAMORPHIC ROCK
-  Metamorphic rocks can form from igneous, sedimentary or other metamorphic rocks.
EARTHQUAKES AND VOLCANIC ACTIVITY CAUSE HEAT AND PRESSURE TO ACT ON ROCKS.
-  sometimes temperature and pressure are great enough to melt rock, forming magma.
-  sometimes pressure flattens mineral grains in rocks without melting them.
-  as pressure and temperature continue to increase over time, one type of rock can change into several different metamorphic rocks.
METAMORPHIC ROCKS ARE  CLASSIFIED BY CLASSIFICATION AND TEXTURE
CLASSIFICATION: 1.  Foliated texture:  mineral grains flatten and line up in parallel layers or bands.
2. Nonfoliated texture:  mineral grains grow and rearrange but do not form layers.
Foliated Rocks ,[object Object],[object Object]
Foliated Rock ,[object Object],[object Object]
Nonfoliated Rock ,[object Object],[object Object]
Nonfoliated Rock ,[object Object],[object Object]
USES OF METAMORPHIC ROCK:  1.  blackboards, roofs, sidewalks, floors:  slate
2.  building stone:  gneiss, marble, quartzite
3.  statues, tombstones:  marble AND GRANITE

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Metamorphic rocks