Quartz is the second most abundant
mineral in the Earth's crust. It has a hexagonal crystal structure
made of triagonal crystallized silica (silicon dioxide, SiO2).
The typical shape is a six-sided prism that ends in six-sided
pyramids, although these are often distorted, or so massive that
only part of the shape is apparent from a mined specimen. Additionally
a bed is a common form, particularly for varieties such
as amethyst,
where the crystals grow up from a matrix and thus only one termination
pyramid is present. A quartz geode consists of a hollow rock (usually with
an approximately spherical shape) with a core lined with a bed
of crystals.
Magmatic
in different types of rocks, mainly in granites, granitic pegmatites
and volcanic rock; metamorphic in different types of rocks, mainly
in quartzites and mica schists; hydrothermal in different types
of ore and Alpine type veins; secondary in oxidation zone of
ore deposits; also in different types of sedimentary
rocks and
in organic remains, also in placers.
Occurence:
Amethyst comes
from Brazil, Uraguay, Mexico, Russia, Thunder Bay area of Canada,
and the United States. Smoky Quartz; Brazil, Colorado, Scotland,
Swiss Alps and China. Rose quartz from Brazil. Citrine is found
with many amethyst deposits. Rock crystal come from Brazil, Arkansas,
Africa. Agate from
Brazil, Lake Superior region, Montana, Mexico and Germany.
Application:
An
important raw material in the glass industry. Gemstones and ornamental
stones