| 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 | |