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Sulfate minerals
Hydrous: gypsum, alabaster | Anhydrous: anhydrite, barite, celestite
Halide minerals
Halite, fluorite
Phosphate minerals
Fluor-hydroxy and chlor-apatite, turqouise
Evaporites
Minerals that precipitate when concentration in water reaches a specific temperature reaches their saturation limit.
Order of precipitation first to last
Calcite, gypsum or anhydrite, halite, potassium and magnesium salts
Structural properties of gypsum
Monoclinic, double columns of tacked [SO4]-2 tetrahedra are linked to columns of Ca+2 and water, columns extend along the c-axis, excellent {010} cleavage, flat prismatic crystals, euhedral crystals.
Chemical formula for gypsum
(CaSO4 * H2O)
Chemical properties of gypsum
Gypsum is hydrous. If water is removed, anhydrite begins to form where gypsum once was.
General properties of gypsum
Pearly luster, hardness 2, common swallowtail twining
Places of occurrence for gypsum
Low-T hydrothermal, major occurrence in evaporitic deposits, grows in cavities
Structural properties of alabaster
Fine grained massive gypsum
Chemical formula for alabaster
CaSO4 * H2O
Chemcial properties for alabaster
Iron impurities make yellow, black or brown veins or patches
Places of occurrence for alabaster
Low pH precipitation, mainly sedimentary with a slightly increased temperature + pressure when forming
Structural properties for anhydrite
Cleavage on (010), (100), (001) planes, individual crystals are rare
Chemical formula for anhydrite
CaSO4
Chemical properties of anhydrite
Alter to gypsum in humid conditions
General properties of anhydrite
White, gray, or lilac color
Places of occurrence for anhydrite
Typical mineral in evaporate deposits, sedimentary precipitation
Structural properties for barite
Orthorhombic symmetry, rhombic-prismatic or tabular in habit, rosette aggregates are common
Chemcial formula for barite
BaSO4
Chemical properties of barite
Solid solution with celestite
General properties of barite
High specific gravity/denstiy
Places of occurrence for barite
Med to Low-Temp hydrothermal deposits
Structural properties for celestite
Orthorhombic symmetry, rhombic-prismatic or tabular in habit, common in druses or aggregates
Chemical formula for celestite
SrSO4
Chemcial properties of celestite
Solid solution with barite
General properties of celestite
Transparent blue color
Places of occurrence for celestite
Hydrothermal, within sedimentary rocks
General properties for halides
Low hardness, high melting point, poor conductor, (some are) soluble
Salt domes
Low density halite NaCl deposits. Intrudes vertically into surrounding rock strata, forming a dome.
Structural properties for halides
Cubic symmetry (CCP), large anions (Cl & F) and metallic cations
Structural properties of halite
Cubic symmetry, {100} cleavage
Chemical formula for halite
NaCl
General properties for halite
Vitreous luster, white or colorless (becomes blue when irradiated with x or gamma rays) or have impurities of Mn (purple), Fe (red), Cu2+(green), hardness 2
Structural properties for fluorite
Cubic coordination polyhedron (cube), 1 F for every 4 Ca, isometric, cube or octahedral crystals, perfect {111} cleavage
Chemical formula for fluorite
CaF2
General properties for fluorite
Vitreous luster, blue, green or violet color, fluorescent in UV, hardness 4
Places of occurrence for flourite
Hydrothermal, common in druses of granite or pegmatites
Structural properties for fluor-hydroxy and chlor-apatite
Hexagonal symmetry, hexagonal prismatic habit
Chemical formula for fluor-hydroxy and chlor-apatite
Ca5(PO4)3 (F, Cl, OH)
General properties for fluor-hydroxy and chlor-apatite
Various colors due to cation substitution, mostly transparent
Places of occurrence for fluor-hydroxy and chlor-apatite
Found in marbles, skarns, and other metamorphic rocks, occurs in igneous rocks and hydrothermal deposits
Structural properties for turquoise
Usually cryptocrystalline
Chemical formula for turquoise
CuAl6(PO4)4(OH)8 * 4H20
General properties for turquoise
Blue to blue-ish green, hardness 6, secondary minerals
Places of occurrence for turquoise
Occurs in veins with altered volcanic rock, often in aggregates