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54 Terms
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Amphibole
-2 cleavage planes at 60 and 120 degrees - Hardness of 6 -Dark green to Black -long, primsatic 6-sided crystals -vitreous to dull lustre -stepped cleavage faces -Double Chain
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Biotite
-Vitreous Lustre -may have faint brown-grey streak -Perfect mica cleavage -1 cleavage plane -Black to brownish Hardness of 2.5-3
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Calcite
-Reacts with HCL -3 Perfect cleavages at 75 degrees - Hardness of 3 - Double refraction and transparent-opaque -Vitreous lustre
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Chalcopyrite
-Goldenyellow or greenish yellow in colour - No cleavage -Black streak -Massive -Hardness of 3.5-4 -CuFeS2
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Dolomite
- 3 cleavages at 75 degrees -Reacts slowly with HCl unless powdered - Vitreous lustre -Small rhombic crystals -Colourless, white, yellow, rarely, gray and blue Hardness of 3.5-4
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Galena
-Dull and Greasy lustre -soils paper and fingers -Grey-Black -1 hardness -1 cleavage plane but not always visble -Black (greenish/brownish) or grey streak -PbS
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Gypsum
-3 cleavage planes (1-perfect with 2-poor/good at 90 degrees) -Tabular/massive or fibrous -Vitreous to silky lustre -White or Colourless -Hardness of 2 CaSO4*2H2O
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Halite
- 3 cleavage planes (perfect at 90 degrees) - Soluble in water -Vitreous and sometime dull lustre Colourless or white -Hardness of 2-2.5
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Magnetite
-Back streak -Dark grey-Black in Colour -No cleavage -dull lustre on non-fresh surface -Attracted to a magnet -Fe2O4 -Hardness of 6
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Muscovite
-1 perfect mica cleavage direction -Colourless to light brown -thin flexible sheets -Transparent -Vitreous lustre -Hardness of 2-3 -light streak
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Olivine
-No cleavage -Hardness of 6.5-7.5 -Olive green to yellow-green -Vitreous to dull lustre -commonly occurs as aggregates of small grains -Transparent to translucent -White Streak
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Plagioclase Feldspar
- 2 cleavage planes of 90 degrees - lamellar twinning -vitreous lustre -Gray-blue-gray -White streak -Hardness of 6
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Potassium Feldspar
- 2 good cleavage planes at 90 degrees -light and dark banding -simple twinning -vitreous lustre -hardness of 6 -salmon-pink, white, gray, green -Hardness of 6
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Pyrite
-Greenish-Black Streak -Hardness of 6-6.5 - brass-yellow colour -Cubic Habit or massive -FeS2
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Pyroxene
2 cleavage directions -light streak -Dark green to black - short prismatic 8-sided crystals -Vitreous to dull lustre -2 imperfect cleavages at 90 degrees -Hardness of 6 -single chain silicate
-Yellow Streak -brown to yellow or black colour -6 perfect dodecahedral cleavage -Resinous lustre
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Sylvite
- 3 cleavage directions at 90 degrees - Hardness of 2.5 -Orange/salmon; reddish; colourless, white, grey -Soluble in water -Bitter taste -Vitreous to dull lustre
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Mohs hardness of 10
Diamond
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Mohs hardness of 9
Corundum
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Mohs hardness of 8
Topaz
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Mohs hardness of 7
Quartz
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Mohs hardness of 6
Orthoclase
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Mohs hardness of 5
Apatite
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Mohs hardness of 4
Fluorite
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Mohs hardness of 3
Calcite
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Mohs hardness of 2
Gypsum
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Mohs hardness of 1
Talc
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Silica Oxygen Tetrahedral
Anion is the silica tetrahedra
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Single Tetrahedral Silicates
Olivine, Forsterite, Fayalite, Zircon, Garnet
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Single Chain Silicates
Augite
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Double Chain Silicates
Hornblende
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Sheet Silicates
Biotite and Muscovite
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Three-Dimensional framework Silicates
Potassium Feldspar and Quartz
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Neosilicates
Isolated silica tetrahedral
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Inosiliates
Chain of silica tetrahedral
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Phyllosilicates
Sheets of silica tetrahedra
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Tectosilicates
3D framework of tetrahedra
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Trends in magnetism (silicates)
The smaller the silicate structure the more magnetic and the larger the structure the less magnetic
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Trends in Mafic behaviour
Smaller the silicate tetrahedra the more mafic
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Clay Group
Sheet silica minerals with water trapped between the sheets
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Kaolinite
Forms china clay
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Serpentine
Formed by metamorphism of basalt
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Quartz Group
Continuously bonded silica tetrahedra
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Feldspar Group
Interlocked Tetrahedra of SiO4 and AlO4 and metal cations
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Zeolites
Interlocking SiO4 and AlO4
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Carbonate Group
Has a Carbonate Radical (CO3)^2
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Sulphate group
SO4
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Native elements
Comprised of a single element
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Sulphides
Minerals with sulfide Sphalerite Chalcopyrite, Pyrite, Galena
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Oxides
Minerals containing oxygen
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Haemetite
-not spontaneously magnetized -major source of iron ore