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ObjectivesObjectivesDescribe seven physical Describe seven physical
properties that help distinguish properties that help distinguish one mineral from another.one mineral from another.
List 5 special properties that may List 5 special properties that may help identify certain mineralshelp identify certain minerals
Physical properties of mineralsPhysical properties of mineralsare a result of the chemical composition and are a result of the chemical composition and
crystalline structurecrystalline structure
Talc is highly variable, yet Sulfur is almost always Talc is highly variable, yet Sulfur is almost always yellowish.yellowish.
TalcTalc
SulfurSulfur
ColorColor: Can be very characteristic for a few minerals, but is not important for others
Talc
Luster:Luster: the way light is reflectedthe way light is reflectedeither either MetallicMetallic or or Non-metallicNon-metallic
Non-metallics are further described as:Non-metallics are further described as:
dulldull(earthy)(earthy) waxy
pearly (translucent)
glassy(transparent)
Hematite has a Hematite has a very very
red streakred streak
Streak:Streak: the color of the color of the powdered mineralthe powdered mineral
CleavageCleavage and and FractureFracturehow a mineral splits how a mineral splits oror how a mineral breakshow a mineral breaks
The Six Crystal SystemsThe Six Crystal Systems
IsometricIsometric OrthorhombicOrthorhombic
TetragonalTetragonal HexagonalHexagonal
MonoclinicMonoclinic TriclinicTriclinic
Isometric SystemIsometric System
Three axes of equal length intersect at 90 degree Three axes of equal length intersect at 90 degree angles.angles.
Examples: Galena, halite, and pyrite.Examples: Galena, halite, and pyrite.
Tetragonal SystemTetragonal System
Three axes intersect at 90 degree angles.Three axes intersect at 90 degree angles. Horizontal axes of equal length.Horizontal axes of equal length. Vertical axis can be longer or shorter than the other two.Vertical axis can be longer or shorter than the other two. Examples: Cassiterite, chalcopyrite, and zircon.Examples: Cassiterite, chalcopyrite, and zircon.
Orthorhombic SystemOrthorhombic System
Three axes of different lengths intersect at 90 Three axes of different lengths intersect at 90 degrees.degrees.
Examples: Olivine, topaz, and staurolite.Examples: Olivine, topaz, and staurolite.
Hexagonal SystemHexagonal System
Three horizontal axes of the same length intersect at Three horizontal axes of the same length intersect at 60 degree angles60 degree angles
The vertical axis may be longer or shorter than the The vertical axis may be longer or shorter than the horizontal axes.horizontal axes.
Examples: Calcite, hematite, and quartz.Examples: Calcite, hematite, and quartz.
Monoclinic SystemMonoclinic System
Three axes of different lengths, two intersect at 90 Three axes of different lengths, two intersect at 90 degree angles.degree angles.
The third axis is oblique (inclined) to the others.The third axis is oblique (inclined) to the others. Examples: Micas, gypsum, microcline (orthoclase)Examples: Micas, gypsum, microcline (orthoclase)
Triclinic SystemTriclinic System
Three axes of unequal length that are oblique Three axes of unequal length that are oblique (inclined) to each other. No 90 degree angles.(inclined) to each other. No 90 degree angles.
Examples: Plagioclase feldspars, turquoise, and Examples: Plagioclase feldspars, turquoise, and axinite.axinite.
We use a scale from 1 to 10 called MOH’S We use a scale from 1 to 10 called MOH’S SCALE OF HARDNESS.SCALE OF HARDNESS.
Talc is a 1 and diamond is a 10. Talc is a 1 and diamond is a 10. Most minerals fall between 3-6. The field Most minerals fall between 3-6. The field
scale can be very helpful:scale can be very helpful:
Field Scale of HardnessField Scale of Hardness
Finger NailFinger Nail 2.5 2.5
PennyPenny 3.5 3.5
Nail or Knife 5.0 to 5.5Nail or Knife 5.0 to 5.5
GlassGlass 5.5 to 6.0 5.5 to 6.0
Specific Gravity (heft):Specific Gravity (heft):
Density = Mass/VolumeDensity = Mass/Volume
SG = Density of Sub./Density of HSG = Density of Sub./Density of H22OO
Dry weight of Mineral SG = ----------------------------------- Dry weight - weight in water
Example low and high Specific GravityExample low and high Specific Gravity
Graphite (low)Graphite (low)
Galena (high)Galena (high)
Magnetism:Magnetism:
Some minerals are attracted to Some minerals are attracted to a magnet.a magnet.
Magnetite
Fluorescence:Fluorescence:Minerals which will glow under Minerals which will glow under
an ultraviolet (black) light.an ultraviolet (black) light.
Minerals that continue to glow after the ultraviolet light is cut off are called phosphorescent.
Opal
Chatoyancy and AsterismChatoyancy and Asterism
Chatoyancy: Silky appearance due to large Chatoyancy: Silky appearance due to large numbers of parallel mineral fibers.numbers of parallel mineral fibers.
Asterism: Six-sided star shape when the Asterism: Six-sided star shape when the mineral reflects light.mineral reflects light.
Radioactivity:Radioactivity:
Some radioactive minerals will Some radioactive minerals will emit charged particles that are emit charged particles that are detected by a geiger counter.detected by a geiger counter.
Uranitite
Malleability:Malleability:
Some minerals Some minerals are bendableare bendable
Some minerals Some minerals are brittleare brittle
GarnetCopper
Feel:Feel:
Some minerals feel greasy or Some minerals feel greasy or soapy (unctuous)soapy (unctuous)
Graphite
Solubility:Solubility:
Some minerals are soluble (will dissolve) Some minerals are soluble (will dissolve) in waterin water
Halite
Double Refraction:Double Refraction:
Optical Optical properties reveal properties reveal a double imagea double image
Iceland Spar (Calcite)