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