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The formation of layers of rock
Stratification
Bodies of water
Course grained
Nonfoliation
More time crystals have to grow, resulting in larger crystals (course grained)
Light colored and less dense
Foliation
Contact
When most of a rock is made of larger grains
Stratification
Bodies of water
Course grained
Nonfoliation
More time crystals have to grow, resulting in larger crystals (course grained)
Light colored and less dense
Foliation
Contact
Metamorphism that occurs when magma directly causes changes and enters rocks' pores
Stratification
Bodies of water
Course grained
Nonfoliation
More time crystals have to grow, resulting in larger crystals (course grained)
Light colored and less dense
Foliation
Contact
Metamorphic rock formation is caused by all of the following except...
Stratification
Bodies of water
Course grained
Nonfoliation
More time crystals have to grow, resulting in larger crystals (course grained)
Light colored and less dense
Foliation
Contact
Mineral grains not arranged in bands.
Stratification
Bodies of water
Course grained
Nonfoliation
More time crystals have to grow, resulting in larger crystals (course grained)
Light colored and less dense
Foliation
Contact
Sedimentary Rocks are usually formed on/near...
Stratification
Bodies of water
Course grained
Nonfoliation
More time crystals have to grow, resulting in larger crystals (course grained)
Light colored and less dense
Foliation
Contact
A felsic igneous rock is...
Stratification
Bodies of water
Course grained
Nonfoliation
More time crystals have to grow, resulting in larger crystals (course grained)
Light colored and less dense
Foliation
Contact
In igneous rocks, the longer it takes to cool, the...
Stratification
Bodies of water
Course grained
Nonfoliation
More time crystals have to grow, resulting in larger crystals (course grained)
Light colored and less dense
Foliation
Contact
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