Pyrite,
or iron pyrite has isometric crystals that usually appear as
cubes or pyritohedrons. Its metallic luster
and pale-to-normal brass-yellow color have earned it the nickname
fool's
gold, but ironically enough, small quantities of actual gold can
sometimes be found in pyrite. In fact, some auriferous pyrite is
a very valuable ore of gold, and others are excellent ores of arsenic,
nickel, cobalt and copper.
Pyrite is often confused with the mineral marcasite.
Marcasite is a polymorph of pyrite,
which means it has the same chemistry as pyrite but a different
structure and, therefore, different
symmetry and crystal
shapes. The marcasite/pyrite polymorph pair
is probably the most famous polymorph pair next to the diamond/graphite
pair. Pyrite is often used in jewelry such as necklaces and bracelets,
but although the two are similar, marcasite cannot be used
in jewelry as it has a tendency to crumble and turn into powder.
Adding to the confusion between marcasite and
pyrite is the use of the word marcasite as a jewelry trade name.
The term is applied to small polished and faceted stones that
are inlaid in sterling silver, but even though they are called marcasite,
they are actually pyrite.
Magmatic
segregations in basic rocks with pyrrhotite and pentlanditie
in pegmatites and skarns; hydrothermal in porphyry and vein
deposits together with other sulfides; hydrothermal,
sedimentary and metamorphic.
Occurrence:
Sudbury,
Ontario, Canada; Park City, Utah, USA; Llallagua, Bolivia; Rio
Tinto, Spain; Navajun, Spain; Climax, Colorado, USA
Application:
Production
of sulfuric acid, used in jewelry under the trade name "marcasite" and
as a mineral specimen