Garnet Mineral Information Page There are six main Garnet Varieties based on ideal end-member garnet chemical compositions:
Some garnets have an intermediate composition somewhere between these end-members like the rhodolite garnet, the
Mozambique garnet, and the malaia garnet varieties.
Some of the named garnet varieties
are of specific colors like the green grossular tsavorite garnet, the yellow-orange to red grossular hessonite garnet, the green andradite variety demantoid garnet, and the intense orange spessartite variety known as mandarin garnet. There also is a very rare color behavior garnet variety known as color change garnet!
Go up to the Garnet Facts and Mineral Information Index Go up to the Garnet Facts and Mineral Information Index Go up to the See all of our natural garnet varieties:
Go up to the The garnets are a group of mineral species all having
essentially the same isometric crystal structure but varying in chemical
composition and in many of their physical properties.
There are six
species of common garnets based on ideal end-member chemical compositions.
These six species are divided into two groups; the pyralspite group
which are the pure chemical end-members Fe3Al2(SiO4)3 (almandine), Mg3Al2(SiO4)3 (pyrope)
and Mn3Al2(SiO4)3 (spessartine), and the ugrandite group or
calcium garnet group consisting of Ca3Fe2(SiO4)3 (andradite),
Ca3Al2(SiO4)3 (grossular),
and Ca3Cr2(SiO4)3
(uvarovite, which actually is not 'common' at all!). Extensive
solid solution occurs within these
two groups, but normally very little substitution occurs between them.
Garnets very
rarely if ever occur in nature with compositions precisely matching the
pure end-member common garnet species (almandine, pyrope,
spessartine, andradite,
grossular and uvarovite).
A natural garnet's composition typically falls somewhere between these end-members,
somewhere within the solid solution ranges for
the pyralspite group or the ugrandite group. Varietal names
have been given to some garnets of intermediate composition
in these solid solution series such as the rose-red to purple rhodolite
garnet, which has a chemical composition averaging a 2:1 mixture of
pyrope to almandine. An additional intermediate variety between pyrope and almandine with a chemical composition
averaging a 1:1 mixture of
pyrope to almandine is the
Mozambique garnet with its beautiful dark orange-red to red color.
Another intermediate composition varietal example is the <malaia garnet which is a yellow to orange to red garnet
variety of an intermediate composition range between spessartite garnet gemstones and pyrope garnet gemstones.
This garnet variety also has a significant grossular component, which
is quite unusual and unexpected due to the significant size difference
between the substituting ions.
The ions Cr3+, V3+ and Ti3+/4+
can substitute in some of the common garnet compositions or occur as trace impurities,
resulting in numerous
less common garnet varieties. Some of these less common garnet varieties
are of specific colors such as the green
vanadium grossular garnet variety tsavorite and the green chromium andradite
garnet variety demantoid. When significant amounts of vanadium and chromium
impurities occur in malaia garnets, a distinct
color change is visible when viewed under fluorescent light versus incandescent light.
Garnets exhibiting this rare color behavior are known as color change garnets.
Grossular garnets of yellow-orange to orange-red to brown colors are known as hessonite
garnets. Some grossular garnet occurs in a translucent massive form known as hydrogrossular with (OH)4-4
substituting for (SiO4)-4 tetrahedra in its crystal structure.
Garnet is allochromatic, meaning that
most of the color variations in different garnets are due to their highly variable trace element impurities rather
than to their bulk composition elements. The color we see in garnets is
produced when light is selectively absorbed
by these ions or by interactions between these ions (intervalent charge
transfers).
It is not possible to determine
the precise species or variety of a garnet based solely upon a comparison of its refractive index and
specific gravity (let alone determining a variety solely by its color!),
although comparing the refractive index and specific gravity can narrow down the possibilities
considerably.
However, methods that rely on specific gravity measurement can be misleading,
because the specific gravity is not only difficult
to measure accurately, but also is prone to error in garnets due to their
abundant inclusions
which can alter their specific gravity considerably.
Perhaps the most reliable method outside of chemical analysis for determining
garnet species and varieties in gem garnets is by comparing their absorption
spectrum, refractive index
and color, which gives a conclusive identification.
Some almandine garnets form with asbestiform mineral inclusions, typically of pyroxene
or amphibole, that give a chatoyant effect yielding a four-ray star when
fashioned into a cabochon gem.
Garnets form in a variety of geologic settings, depending on the garnet species.
Almandine typically occurs in schists and gneisses, resulting from
regional metamorphism of argillaceous sediments. It is a characteristic mineral
constituent of the amphibolite metamorphic facies, also appearing in
the granulite facies. Almandine also occurs in pegmatite dikes and in some
granitic and volcanic rocks, as well as in sedimentary deposits as detrital grains.
Pyrope is characteristic of ultra-mafic rocks such as peridotites,
kimberlites, eclogites, and serpentines, and in sedimentary deposits derived
from their weathering.
Spessartine occurs occaisionally in granitic pegmaties and in skarns, also
found in sedimentary deposits.
Andradite commonly occurs in contact metamorphic deposits,
resulting from metamorphism of impure limestones. It also is found in some
metasomatic skarn deposits. The light colored andradite varieties topazolite and
demantoid occur mainly in serpentinites and chlorite schists. The darker
andradite varieties melanite and schorlomite occur mainly in alkaline
igneous rocks such as nepheline syenites and phonolites.
Grossular occurs mainly in contact and regional metamorphic deposits,
resulting from metamorphism of impure limestones. It also has been found in
alkaline igneous rocks, and has been reported in pegmatites and hydrothermal veins.
Uvarovite is a rare garnet occurring in peridotite and serpentinite
associated with chromite.
Garnets are usually recognized by their form, color and hardness. The garnet varieties
can be distinguished by their refractive index, absorption spectrum and color. Another method
utilizes specific gravity, refractive index and unit cell dimension.
The name garnet is from the Latin word granatus which originated
when garnet grains in rock were compared to the dark red seeds of the
pomegranate fruit.
Garnets have been used as gemstones for many thousands of years. In ancient
times they were known as carbuncles, as were other red gems.
They were in the 'Breastplate of Judgement' of
Aaron, described in the bible (Exodus: xxviii, 15-30). The Koran states that the fourth heaven is
composed of carbuncle. In Vedic astrology ( 1000's of years older than western
astrology and still practiced by millions today), the brownish-orange/red hessonite garnet
has long been a preferred talisman for warding off the evil influences of the celestial body named Rahu. Garnet was
considered a sacred stone by many native indian tribes
of North, South and Central America.
Garnet is the birthstone for the month of January.
The following properties are attributed to some of the specific garnet varieties:
For additional metaphysical properties of garnets,
see our Metaphysical Books section.
This is the end of our Garnet Factsheet and Mineral Information page.
Enter our Virtual Gallery of See our Don't miss our Gallery of
and
MINERALMINERS.COM® - Your Personal 'Link' Direct to the Mines for Garnets!TM
Garnet: Mineral Information & Garnet Facts
Garnet Mineral Information Topics On This Page:
Natural Garnets
Garnet Varieties & Natural Garnet Merchandise
Garnet Product Categories in Our Online Store
Garnet Product Groups in Our Virtual Gallery:
(Follow any link to enter our Online Store)
GARNET PHYSICAL PROPERTIES
Varieties of GARNET
GARNET BACKGROUND INFORMATION
In most cases, unit cell dimension measurements can be compared with the refractive
index and specific gravity to determine chemical composition in terms of major end-members.
In the absence of chemical analysis some
ambiguitiy will often still exist, leaving one to rely on additional information such as
occurance, associated minerals and color.
Go up to the Garnet Facts and Mineral Information Index
GARNET GEOLOGIC OCCURRENCE AND DIAGNOSTIC FEATURES
Go up to the Garnet Facts and Mineral Information Index
GARNET HISTORICAL INFORMATION AND USES
Pyralspite is derived from the names of the three garnet species in
its group: PYRope, ALmandine, and SPessartine, with 'ite' added to the end.
Ugrandite is derived from the names of the three garnet species in
its group: Uvarovite, GRossular, and ANDradite, with 'ite' added to the end.
Almandine was named after the ancient locality Alabander in Asia minor, where
once many garnets were cut and polished.
Pyrope is from the Greek for fire-like, refering to its color.
Spessartine was named for a locality in the Spessart district in Bavaria.
Andradite was named after the Portuguese mineralogist d'Andrade.
Grossular was named after the gooseberry R. grossularia,
because of the similar pale green color of the original specimens.
Uvarovite is named after the Russian mineralogist Count Sergei Simonovitch Uvarov.
Rhodolite is from the Greek rhodon meaning rose, refering to its color.
Malaia is from the Swahili word malia meaning
out of the family, refering to the fact that this garnet variety
typically has some distinctively different physical properties than other
garnets found in the same area.
Tsavorite is named after the Tsavor Game Preserve of Kenya, near which it was discovered.
Demantoid is from the French demant meaning diamond,
in allusion to its similar brilliance.
Melanite is from the Greek melanos meaning black,
refering to its color.
Topazolite named after its similarity to yellow topaz.
In 1892, the Hunzas used bullets made of garnet against the British troops
in Kashmir, believing them to be more deadly than lead.
Historically, garnets were believed to give protection from wounds and
poison, to stop bleeding and to symbolize truth & fidelity, and bring prosperity.
As gemstones, garnets today are more popular than ever. Some of the
newer varieties such as tsavorite garnet gemstones have only become available in the last century.
Garnets are also used today for a number of abrasive purposes.
Garnet is the symbolic gemstone for the 18th wedding anniversity.
The astrological signs of garnet are Leo, Virgo, Capricorn and Aquarius.
Go up to the Garnet Facts and Mineral Information Index
GARNET METAPHYSICAL PROPERTIES
Garnets are said to enhance creativity and understanding, and
to bring success in business. They also are said to strengthen willpower and
increase self-esteem and popularity.
Garnets are also said to help in the treatment of infectious diseases,
blood poisoning, and heart & lung diseases.
Almandine is said to be particularly usefull for strengthening the heart,
to inspire love and to perceive truth.
Andradite is said to give vitality and to help prevent
fears, insecurity, and feelings of loneliness.
Pyrope is said to enhance understanding and wisdom.
Rhodolite is said to facilitate meditation and enhance intuition, and to inspire love.
Tsavorite Gemstones are said to facilitate meditation, and to enhance spiritual awareness and
telepathic abilities.
Last Updated: July 18, 2020
Garnet Jewelry - Earrings
© Copyright 1998, 1999, 2000, 2001, 2002, 2003, 2004, 2005, 2006, 2007, 2008, 2009, 2010, 2011, 2012, 2013, 2014, 2015, 2016, 2017, 2018, 2019, 2020
Gem & Mineral Miners, Inc.® All Rights Reserved.