Igneous
When magma cools and solidifies through process of crystallization
Extrusive (volcanic rocks)
Molten rocks that solidify
Intrusive (plutonic rocks)
Formed at depth
Characterization: Texture and crystal size
TYPES OF IGNEOUS ROCKS BASED ON TEXTURE |
Coarse-grained or Phaneritic
Fine-grained or Aphanitic
Porphyritic
Glossy-textured
Felsic
Mafic
Andesitic
Ultramafic
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Sedimentary
Sediments result from uplift and weathering, which then transported and deposited in different areas
Lithification
Sediments are transformed into solid sedimentary rocks
Compaction
Files of sediments accumulate and materials below are compacted by the weight of the overlying layers
Cementation
Water that seeps through pore spaces, containing cementing materials which binds particles together
Common cements
Calcite, silica, iron oxide
Strata
Characteristic where fossils or imprints or animals that existed are seen
TYPES OF SEDIMENTARY ROCKS |
Detrital sedimentary rocks
Chemical sedimentary rocks
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Metamorphic
Came from pre-existing rocks
Parent rocks undergo changes in mineralogy, texture, and chemical composition
Subjected to high heat and pressure
Metamorphism
Transformation of parent rock into texturally and mineralogically new rock
Heat
Most important agent of metamorphism
Stress
Another agent
Foliation
Tectonic forces squeeze rocks as they are heated, rocks deform into folds and form layers
Pressure
Causes spaces to close, producing a more compact rock
Chemically-active fluids
Water, carbon dioxide, volatile materials
Catalysts to promote crystallization
TYPES OF METAMORPHIC ROCKS |
State
Gneiss
Marble
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