Composed primarily of silicon-oxygen tetrahedrons (SiO42−)
Silicate minerals
Olivine (Mg, Fe)2SiO4)
Feldspar (KAlSi3O8)
Pyroxene, Amphibole, Muscovite
Oxides
Consist of metal cations bonded to oxygenanions(O2−)
Sulfides
Consist of metal cations bonded to sulfides(S2−)
Sulfates
Consist of metal cations bonded to sulfate(SO42−)anionic groups
Sulfate minerals
Gypsum (CaSO4 ∙ 2H2O)
Barite / Baryte (BaSO4)
Halides
Consist of metal cations bonded to halogens
Halide minerals
Halite / Rock salt (NaCl)
Fluorite (CaF2)
Carbonates
Consist of minerals with carbonic ion present that easily bond with metals
Carbonate minerals
Calcite (CaCO3)
Dolomite (CaMg(CO3)2)
Natives / Nativemetals
Consist of singular metal elements in pure form
Native metal minerals
Copper (Cu)
Gold (Au)
Bismuth (Bi)
Crystal structures
Isomeric
Monoclinic
Orthorhombic
Tetragonal
Hexagonal
Triclinic
Isomeric
Common crystal system whose unit cell is in the shape of a cube (𝑎1 , 𝑎2 , 𝑎3 )
Monoclinic
Crystal structure whose axes [(x, y, z) OR (a, b, c)] have different lengths; both x- and z-axes meet at 90° while the y-axis does not
Orthorhombic
Crystal structure whose axes [(x, y, z) OR (a, b, c)] have different lengths; all three (3) axes meet at 90°
Tetragonal
Crystal structure whose two (2) axes [(𝑥1 , 𝑥2 ) OR (𝑎1 , 𝑎2 )] have equal lengths while the third axis (𝑧 OR 𝑐) is longer; all three (3) axes meet at 90°
Hexagonal
Has 4 crystallographic axes consisting of 3 equilateral axes angling at 120° to each other, with 1 perpendicular axis
Triclinic
The rhombohedron system - crystal system that is similar to the isometric system, but it has been skewed to 1 side, making it oblique