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13 Cards in this Set

  • Front
  • Back

-Muscovite


-Perfect cleavage in 1 direction


-H=2.5 on cleavage surfaces, around 4 at a right angle to cleavage


-Crystals have a platy 'micaceous' habit


-Individual plates tend to be elastic


-Crystals are often clear and light grey to silvery, & may be tan or light brown


-Biotite


-Perfect cleavage in 1 direction


-Crystals tend to occur with a platy 'micaceous' habit


-Individual plates tend to be brittle


-Crystals are often deep brown, and may be reddish brown to black


-Talc


-Platy habit is common


-H=1


-Masses of crystals have a soapy, smooth feel


-Crystals are commonly white to clear, & may be light green


-Kaolinite (Clay)


-Crystals are usually smaller than mm-scale to microscopic


-Occur in white, chalky masses


-Earthy odor when damp


-H=2.3


-Orthoclase (Feldspar)


-Prominent cleavage in 2 directions that are close to 90 degrees apart


-H=6


-May be clear, white, tan, pink, red, or brown


-Crystals may contain thin layers of lightly colored plagioclase (perthitic texture)


-Plagioclase (Feldspar)


-Prominent cleavage in 2 directions that are close to 90 degrees apart


-H=6


-May be clear, white or grey


-One cleavage plane may show thin parallel striations (twin planes)


-Kyanite


-Perfect cleavage in 1 direction


-Commonly has a bladed habit


-H=5 along crystals & H=7 across crystals


-May be colorless, grey or cyan (blue)



-Augite (Pyroxene)


-Prominent cleavage in 2 directions that are close to 90 degrees apart


-Common chemical varieties are dark green to black


-H=6.5


-Hornblende (Amphibole)


-Prominent cleavage in 2 directions that are close to 60 or 120 degrees apart


-Common chemical varieties are dark green to black


-H=6


-Quartz


-Conchoidal fracture (breaks into curved surfaces)


-H=7


-Crystals are hexagonal with prism and pyramid forms common


-May be clear, white, smoky, purple, or yellow-brown



-Garnet


-Irregular fracture


-H=7


-Commonly deep red but may be purple, green, black, or white


-Crystals are commonly equant with dodecahedron forms


-Staurolite


-Irregular fracture


-Earthy luster when weathered


-H=7


-Crystal faces display prominent 90 degree angles


-Twinned crystals are common


-Typically deep red brown to brown in color


-Olivine


-Irregular to conchoidal fracture in large crystals


-H=6.5


-May be cm-scale single crystals or sugary masses of small crystals


-Typically bright green & may show shades of brown to yellow