A sulphate which may contain traces of calcium and
barium. It is usually sky blue in colour but may also be white/brownish
yellow. It is the main source of strontium which is used in fireworks
and flares because it burns with a red flame.
It is also used in the manufacture of varnishes
and household ceramics.
It is easily scratched (3-3.5 on the mohs scale) and
derives it's name from it's celestial blue colour.
It is found in granites and pegmatites and may also
be formed by the evaporation of salt water in closed basins. Here it
exists with chalk and aragonite.
It is fairly common and was first discovered in Sicily
in 1781. (Here it occurs in chalk and is usually white). The finest
samples are now found in US. It may also be found in Russia, Tunisia,
and UK (Gloucestershire).

A carbonate which is very beautiful but too soft to
be used as a gemstone (3-3.5 on the mohs scale). It is very brittle
and fragile. It is usually colourless or white but may also be blue/green/grey.
It is a minor source of lead but is rarer than galena which is the main
source.
It is a secondary mineral which forms by the alteration
of galena in oxidised zones of lead veins. It may be found in association
with galena, smithsonite and sphalerite. It usually forms in needle
like shapes (acicular). Arrow head shaped crystals
are very common. These form due to twinning which is when two crystals
grow into each other.
It's name is derived from the Greek word keros which
means wax.
The largest crystals were found in Namibia (over 10cm
long). It can also be found in Sardinia, Australia, Siberia, Tunisia,
US and Scotland (Strathclyde region).
