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Mineral IdentificationThe Sulfides
These are not common minerals but are prized because of their economic value.
Geologists often make these minerals the target of their exploration.
These minerals are the source of many metals we use today.
These minerals must be refined to separate the metal from the sulfur
The properties they share are metallic lustre, high specific gravity (heavy) and streak.
The Sulfides
Remember to streak all metallic minerals Have a magnet handy as some sulfides are
magnetic. Remember to wash your hands after
handling due to the presence of heavy metals.
Identification notes
PROPERTY
Colour Caramel brown to Black
Crystal Form rare
Cleavage/Fracture Common in 6 directions – as a result the small grains have many smooth cleavage faces which cause the mineral to sparkle!
Lustre Sub-metallic – can be somewhat vitreous
Hardness Soft (4)
Specific Gravity heavy
Streak Brown to black (few minerals streak brown – the other you know is Chromite)
Other Commonly found with Galena (and even Chalcopyrite) in limestone.It is the main ore of zinc (used to galvanize steel)
19) Sphalerite (ZnS)
PROPERTY
Colour Brassy yellow
Crystal Form Common (cubes, pyritohedrons, striated crystals) but is usually seen massive
Cleavage/Fracture none
Lustre Metallic
Hardness Very hard (7) – can scratch glass – unusual for a metallic mineral
Specific Gravity Medium-heavy
Streak black
Other Non-magneticThe most common metallic mineral !– often called “fools gold” due to its brassy colour (this mineral shares almost no other properties with gold)Despite its abundance it has no economic value – most iron ores are iron oxides. It is indicator mineral in many gold mines.
20) Pyrite (FeS2)
PROPERTY
Colour Gun-metal grey
Crystal Form Common (cubes, pyritohedrons, striated crystals) but is usually seen massive
Cleavage/Fracture Perfect in 3 directions 90˚ creating cubic cleavage fragments
Lustre Metallic – very lustrous cleavage faces
Hardness Soft (3) – soft – easily scratched by a nail
Specific Gravity Very heavy due to the lead – densest mineral in our set.
Streak black
Other Commonly associated with sphalerite.Galena “rusts” to a duller greyNon-magneticIt is the main ore of lead in the world
21) Galena (PbS)
PROPERTY
Colour Yellow-gold – the colour is more yellow than pyrite but less golden than gold.
Crystal Form Almost always massive
Cleavage/Fracture none
Lustre Metallic
Hardness hard (4.5) – cannot scratch glass – can be scratched with a nail
Specific Gravity Medium-heavy
Streak black
Other Non-magneticThe problem is that it is often associated with pyrrhotite which is magneticIt is a major ore of copper. Used for wiring and pipes.
22) Chalcopyrite (CuS2)
PROPERTY
Colour Brownish metallic
Crystal Form Usually massive but can form hexagonal prismatic crystals.
Cleavage/Fracture none
Lustre Metallic
Hardness hard (5) – cannot scratch glass – can be scratched with a nail
Specific Gravity Medium-heavy
Streak black
Other MagneticIt is often associated with similarly coloured pyrite and chalcopyriteOdd formula is due to Fe atoms that are often absent in the crystal structure.It has little economic value
23) Pyrrhotite (Fe1-xS)
PROPERTY
Colour Black sub-metallic to purplish metallic with a common irridescent coloured surface leading to its nickname of “Peacock Ore”
Crystal Form Usually massive
Cleavage/Fracture none
Lustre Metallic-Sub-metallic
Hardness soft (4) – cannot scratch glass – can be scratched with a nail
Specific Gravity Medium-heavy
Streak black
Other Non-MagneticAlmost always has a greenish “rust”It is often associated with other copper sulfides such as chalcopyriteIt is a secondary ore of copper
24) Bornite (Fe5CuS4)