Crystals are rare and thus bornite is usually
known as a massive mineral ore.
It does however get used in the mineral trade
as a curiosity called "peacock ore". A favorite among
children, the bornite chunks sold as peacock ore or alternatively
peacock copper have a rich bouquet of colors. The colors are from an
iridescent tarnish that forms on bornite upon exposure to air. The
tarnish is made of assorted copper oxides or hydroxides that form a
mere atoms thin layer over the bornite. The thickness of the layers
is close to the wavelength of light. When light waves bounce between
the bornite surface and the top of the tarnish layer they will leave
with the wavelengths of various colors. This effect is the same as
the rainbow effect that occurs with oil on water. In the case of
bornite, the tarnish will have a purplish, violet or blue color.
Because bornite is often intergrown with chalcopyrite which tarnishes
to more greens and yellows, the peacock ore may have many colors
ranging from purple to blue to green to yellow.
Bornite at Tsumeb
Cu5UeS4 Forms massive areas
of a copper-to pinchbeck-brown color which tarnish rapidly, the
purplish blue characteristic of bornite. Crystals have very rarely
been found. Some bornite contains up to 1.5 kg of silver per ton.
Borrnite is also a rather rare mineral at
Tsumeb. In contrast to the upper levels it is found in greater
abundance at greater depth. Massive pieces of about 1 cm in size
occur with germanite