ROCK CYCLE


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

  • Large crystals that are visible to the eye


Fine-grained or Aphanitic

  • Small crystals that cannot be seen by the naked eye


Porphyritic

  • Large difference in grain size

  • Large grain (phenocryst)

  • Finer grain (groundmass/matrix)


Glossy-textured

  • Non-crystalline and no mineral grains


Felsic

  • Rocks with light color


Mafic

  • Dark in color


Andesitic

  • Light and dark color


Ultramafic

  • Mostly dark-colored



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

  • Weathered rocks

  • Basis: size or particles


Chemical sedimentary rocks

  • Weathered rocks

  • Basis: chemical composition



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

  • Foliated, fine-grained

  • Parent rock: shale


Gneiss

  • Foliated, medium to coarse-grained

  • Parent rock: granite, volcanic rock


Marble

  • Non-foliated, medium to coarse-grained

  • Parent rock: limestone

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