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16 Cards in this Set

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Granite

CC: Felsic


DM: Quartz, Potassium, Feldspar


RM: Micas, Amphibole


C: 0-25%

Rhyolite

CC: Felsic


DM: Quartz, Potassium, Feldspar


RM: Micas, Amphibole


C: 0-25%

Vesicular Pumice

Pyroclastic


Very vesicular

Diorite

  • CC: Intermediate (Andestic)
  • DM: Amphibole, Plagioclase Feldspar
  • RM: Pyroxene, Biotite
  • C: 25-45%

Andesite

  • CC: Intermediate (Andestic)
  • DM: Amphibole, Plagioclase Feldspar
  • RM: Pyroxene, Biotite
  • C: 25-45%

Porphyritic Andesite

Aphanitic rocks that contain scattered coarse or medium phenocrysts surrounded by groundmass composed of fine crystals &/or glass. This texture is sometimes formed by a two stage cooling system.

Gabbro

  • CC: Mafic (Basaltic)
  • DM: Pyroxene, Plagioclase Feldspar
  • RM: Amphibole, Olivine
  • C: 45-85%

Basalt

  • CC: Mafic (Basaltic)
  • DM: Pyroxene, Plagioclase Feldspar
  • RM: Amphibole, Olivine
  • C: 45-85%

Vesiclular Basalt

Bubbles which result in holes in the completely solidified rock.

Bubbles which result in holes in the completely solidified rock.

Amygdaloidal Basalt

 


Vesicles that have been filled with a secondary mineral long after the flow cooled ( commonly quartz or calcite )

Vesicles that have been filled with a secondary mineral long


after the flow cooled ( commonly quartz or calcite )

Obsidian

Pyroclastic


Volcanic glass

Peridotite

  • CC: ultra-Mafic
  • DM: Pyroxene, Olive
  • RM: Plagioclase Feldspar
  • C: 85-100%

Komattite

  • CC: ultra-Mafic
  • DM: Pyroxene, Olive
  • RM: Plagioclase Feldspar
  • C: 85-100%

Phaneritic Igneous Rocks

Igneous rocks in which all the crystals are large enough to be distinguished, Medium to coarse crystals. Also called intrusive or plutonic because they form below the surface.

Pyroclastic

Rocks that are formed by the ejection of molten rocks into the atmosphere

Aphanitic Igneous Rocks

Rocks that form by the rapid cooling lava, at or near the surface. They have a fine crystal size. Also called extrusive or volcanic.