Some
Metallic
Minerals and their
Characteristic Properties

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NAME
FORMULA
HABIT LUSTRE
S.g.
USUAL COLOUR/
STREAK
HARDNESS
CLEAVAGE
OTHER
PROPERTIES
OCCURRENCE
USES
Galena

PbS

cubic crystals metallic

7.5

silver-grey

grey-black

2.5

3; perfect cubic cleavage

vein mineral, often with calcite, fluorspar and barites

cheif source of lead (Pb).

Haematite

Fe2O3

reniform aggregate habit earthy

5

Red-brown

red-brown

5.5 to 6.5

2 poor cleavages

sub-conchoidal or uneven fracture often in limestones as a relacement minerals, also in metamorfphic deposites, ironstones and as both thin veins and cement in sandstones eg. the New Red Sandstone

iron ore and used as a pigment in paint 'Red Ochre'

Pyrite

FeS2

cubic crystals, or as pentagonal dodecahedral crystals.  Also as nodules with an internal structure of radiating needles, also as crystalline masses metallic

5.0

brass-yellow

black

6 - 6.5

no cleavage

cubic crystals often have striated faces,
conchoidal fracture, 
sparks when struck with geological hammer 
pyrite = fire mineral.
smells sulphurous when rubbed on a streak plate
occurs as free crystals or nodules in coal, clay and shales, also in veins

formerly source of sulphur, used to make sulphuric acid (native sulphur now main source).

Sphalerite (aka zinc blende, black jack)

ZnS

usually massive aggregates, also tetrahedral crystals resinous, sometimes brilliant or adamantine on fresh surfaces

4.0

brown or black

pale yellow

3.5 - 4

perfect cleavage in 6 directions

smells sulphurous when rubbed on a streak plate vein mineral

chief source of [non-corrosive] zinc, used for galvanisation of iron

Chalcopyrite

CuFeS2

octohedral and tetrahedral crystals metallic

4.1 - 4.3

brass-yellow

black or greenish-black

3.5 - 4.0

indistinct

ore mineral

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