A sulphide which is grey in colour and is the
main industrial source of lead. The name galena is the Latin word for
lead ore. It is also known as lead glance.
Lead is soft, dense, heavy and a poor conductor of
electricity. It is also very malleable and can be easily flattened into
sheets. Most lead is used for batteries but it is also used for solder
and ammunition. Lead is very poisonous. In recent years health problems
have resulted in the UK when lead from old pipes has contaminated drinking
water.
Galena is very common and widely distributed. It is
found in hydrothermals and sedimentary rocks and also in dolomites and
limestones. It reacts easily with oxygen to form cerusite, mimetite
or pyromorphite.
It may be found in New South
Wales, Australia, Germany, Sardinia and Missouri and Oklahoma (US).
It may also be found in Derbyshire, Cornwall and Derbyshire (UK).
A silicate which is very variable in colour. It may
be black, brown, green, orange, pink or red and has a glassy to greasy
sheen. It may be classed as a neosilicate. These minerals contain silica
molecules which are isolated from one another within their structure.
It is very hard (6-7.5 on the mohs scale) and is therefore
used as an abrasive. It may also be used in jewellery. Garnets have
a very complex chemical composition with the proportion of metals varying
from specimen to specimen.
Grossular garnet was discovered in Siberia in the early
1800's. Grossular is derived from the Latin word grossukaria which means
gooseberry and refers to the green colour of the first specimen identified.
It forms by contact metamorphism and can be found in
limestone rocks that have reacted with hot molten rock (magmatic inclusions).
It may also be found in some igneous rocks.
Grossular garnet can be found in Canada, Italy, Mexico,
Pakistan and Switzerland. Hessonite (also known as cinnamon stone) is
a brown variety of grossular garnet that comes from Sri Lanka and Tanzania.
Vanadium is another variety from Kenya.