Chrysoprase is a green variety
of chalcedony quartz (also known as prase). Like quartz it is composed
of one atom of silicon and two of oxygen and is therefore a form of
silicon dioxide.
It is green due to the presence of small particles
of hydrated nickel sulphate. This becomes incorporated into the gemstone
when it first solidifies and is usually spread evenly throughout it.
Although it is fairly hard (7 on the mohs scale) it is brittle and it's
colour may fade after a long time of exposure to the sun.
Chrysoprase is mainly used for
jewellery. It's green colour is sometimes enhanced
in order to increase it's value. It may be substituted by yellow chalcedony
which can be dyed green with chromium or nickel salts.
The finest samples are found in Australia
but it may be also be found in Poland, Czech Republic, Russia, California,
Brazil and Austria.

CITRINE
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A very common form of quartz which is usually yellow
but may also be brown/orange. It is fairly hard (7 on the mohs scale).
It derives it's yellow colour from oxides of ferric iron but apart from
this it is almost free from inclusions. It's colour is usually consistent
throughout.
It forms in many parts of the world when quartz melts
and then resolidifies with inclusions of iron. It's name is derived
from the Greek word kitros which means lemon. It is usually classed
as an oxide but is also a silicate because it is an oxide of silicon.
Although it rarely has a strong enough colour to be
used for jewellery if it is heated it may become pink and can then be
used to simulate topaz. Citrine may itself be simulated by amethyst
because when this is heated it changes colour from purple to yellow.
(It is this type of citrine which is usually found in shops in the UK)
This would not have occurred years ago because amethyst was more valuable.
It's value declined dramatically after the discovery of amethyst in
Brazil and Uruguay at the end of the 19th century.
Some gemstones are made up of a naturally occurring
combination of amethyst and citrine. These are known as ametrines.
It may be found in igneous, sedimentary or metamorphic
rocks. It may be found in Brazil, France, US and Russia.
