Unlike minerals such as beryl or corundum that are a single species with colored varieties created by trace elements, garnets come in different species and are never found in their pure state. They are always mixed with other garnet species. Garnets are called a solid-state series or a blend. Some of these blends have distinct features and are recognized as varieties of garnets in themselves. What makes them all garnets is the same crystal structure and similar properties.
Although these garnets have very similar colors, they belong to different species and blends. Almandines: Brazil (6.4); Idaho (1.8); Rhodolites: Zimbabwe (4.81); Uganda (1.86); Kenya (3.3); Pyrope (3.71). Photo © Joel E. Arem, PhD, FGA. Used with permission.
For more information on these species and their own varieties, click on the links to the individual listings.
The most common gemstone in the garnet family, almandines come in a wide range of colors. The blend of almandine-pyrope is the dark red variety popularly associated with garnets.
One of the rarest garnets, andradites have the highest dispersion of all garnets, with even more fire than diamond. Demantoids, a variety of andradite, are especially prized.
Salamander pin, featuring 38 diamonds and 28 demantoids, circa 1895. Photo © Joel E. Arem, PhD, FGA. Used with permission.
Unlike other garnets, grossulars are rarely red or dark in tone. However, they do occur in every color, even colorless, except blue. Their light to medium tones and vibrant colors make them excellent jewelry stones. Tsavorites have an emerald-like green color and can command high prices, while hessonite “cinnamon stones” are popular and inexpensive.
Grossular garnet, Asbestos, Quebec, Canada (9.81). Photo © Joel E. Arem, PhD, FGA. Used with permission.
Never transparent, hydrogrossulars are commonly blueish green in color but are sometimes found in pink, white, and gray. (Editor’s note: the classification of hydrogrossular as a garnet species is debatable).
Hydrogrossular cabochon, 13.03 cts, 16.7 mm, Peru. © The Gem Trader. Used with permission.
Chrome pyropes show a red that can rival rubies. However, these stones have a very dark tone.
Chrome pyropes from Arizona are sometimes called “anthill garnets,” because ants can bring these stones to the surface. Round brilliant-cut chrome pyrope, 1.79 cts, 7.5 mm, Garnet Ridge, Near Dinnehotso, Apache Co., Arizona. © The Gem Trader. Used with permission.
Also known as spessartines, spessartites are somewhat rare garnets. They come in a variety of orange colors. Mandarin garnets, a variety of spessartite with a striking orange color, are highly sought.
Spessartites. Photo © Joel E. Arem, PhD, FGA. Used with permission.
The rarest member of the garnet family, uvarovites have a dark, rich green that rivals emerald. Facetable material is even rarer and always small.
Non-Gem Garnet Species
Non-gem garnet species include goldmanite, henritermierite, kimzeyite, majorite, schorlomite, and yamatoite. These garnets may interest collectors of rare mineral specimens.
This large vug contains crystals of grayish white nepheline and jet-black schorlomite. 6.0 x 4.4 x 3.8 cm. Bou-Agrao Mt., Tamazeght complex, High Atlas Mts, Khenifra Province, Meknes-Tafilalet Region, Morocco. © Rob Lavinsky, www.iRocks.com. Used with permission.
The following blends are considered to be varieties of garnet and not sub-varieties of the above species.
Rhodolites are a blend of pyrope and almandine with a distinctive purplish color.
Rhodolite garnet (24.46). Photo © Joel E. Arem, PhD, FGA. Used with permission.
Malaya or Malaia Garnet
This term was originally used to describe garnets that didn’t fit into standard categories. Now, gemologists recognize malaya or malaia garnets as a blend of pyrope and spessartite.
Malaia garnets Photo © Joel E. Arem, PhD, FGA. Used with permission.
Color Change Garnet
In recent decades, color change garnets have been discovered that turn blue in artificial light. In the late 1990s, blue garnets that are red with purple flashes under incandescent light were discovered in Madagascar. These color change stones are a pyrope-spessartite blend. Some Idaho garnets show a strong color shift from red to purplish red. These are an almandine-pyrope mix.
This purple pyralspite garnet shifts to red color under incandescent and LED light. © Bear Williams, Bear Essentials Inc. Used with permission. Re-cropped.
The following species are known to blend:
- Andradite-grossular (also known as grandites or Mali garnets)
Identifying garnets is complicated. In the last fifty years, several new blends have been discovered in East Africa. There’s no reason to believe that all the possible blends have been discovered. We don’t know what the future holds for gemologists.
Garnets share common properties at the molecular level despite considerable variations. For those not scientifically inclined, here’s a visualization that, while not scientifically rigorous, may help illustrate this. If your hand were a model of a garnet molecule, all garnets would share the arrangement of atoms represented by the palm. However, the atoms represented by your fingers are interchangeable. In other words, different atoms can reside on your fingers, while the palm remains the same. Anytime you change the chemistry, you have a different species. Change the atoms of a finger and you have a different species, even though the structure and related properties remain the same (or very nearly so).
Of course, the chemistry of garnets varies far more than the hand model can accurately demonstrate. Below is the chemical composition of the gem garnet species.
- Almandine: Fe3Al2Si3O12
- Andradite: Ca3Fe2Si3O12
- Grossular: Ca3Al2Si3O12
- Hydrogrossular: Ca3Al2(SiO4)3-x(OH)4x
- Pyrope: Mg3Al2Si3O12
- Spessartite: Mn3Al2Si3O12
- Uvarovite: Ca3Cr2Si3O12
As you can see, there are several variations in chemistry. Nevertheless, they all maintain the same basic structure. Garnets crystallize in the isometric system. Their most common forms are the trapezohedron and dodecahedron. Curiously, they rarely appear as cubes or octahedrons, the most common shapes of other isometric minerals. Garnets may also be massive, granular, and in tumbled pebbles.
For decades, gemologists have described rhodolite as one part almandine and two parts pyrope. However, garnets are not that simple. Rhodolite gems, as well as all other garnets, have some of the other species in the mix as well. These may be present in very small amounts, but garnets are never as simple as just two ingredients. Furthermore, a solid-state series like an almandine-pyrope blend doesn’t mean that it’s a mix of two kinds of molecules, Fe3Al2Si3O12 and Mg3Al2Si3O12. Instead, it means that the structure contains both Fe and Mg.
Are There Any Pure Garnets?
In nature, garnets don’t form as a single pure species. The purest gem-quality pyrope ever discovered contained about 83% pyrope, 15% almandine, and about 2% other garnets. The same is true for almandine and grossular. 80% is about the purest you’ll encounter. However, andradite and spessartite garnets have been found as high as 95% pure. Non-gem sized, colorless garnets of 97% pure pyrope have been found. It’s something to give the lover of garnets (or purity) hope.
Almandite or almandine? Spessartite or spessartine? Originally, British gemologists preferred spellings ending with “-ite.” Their American counterparts used “-ine.” Over the last century, the distinction became blurred. Today, both variations are acceptable throughout the world. Almandine and copper ring, jewelry and photo by Paul Reyes. Licensed under CC By-ND 2.0
Garnets were traditionally described as a straight-line series, such as almandine-pyrope or pyrope-spessartite. However, this is not accurate enough to explain the complex blends we now see.
A more useful description is a two-dimensional graph, with almandine, pyrope, and spessartite marking the three corners.
A gem’s chemistry would rarely be located on one of the flat sides. In actuality, it would be a point inside the triangle, indicating how much of each element is present.
For complete accuracy, a three-dimensional model works best. This can add andradite, grossular, and uvarovite to the formula.
While less common, grossular and andradite occur in almost all garnet blends. With this graph, one can indicate how much of each of these species is present in an individual specimen.
It’s important for gemologists to understand garnet blends. The garnets known today show considerable varieties in their mixtures. For identification purposes, standard practice is to name garnets by their two primary species unless it’s a common variety. Just understand that garnets aren’t simple, two-species minerals.
In the past, gemologists have grouped garnets according to chemical composition. This nomenclature persists. Garnets that contain Al (aluminum) in the B position in their chemical formula are known as pyralspites (for pyrope, almandine, and spessartite). Garnets with Ca (calcium) in the A position are known as ugrandites (uvarovite, grossular, and andradite).
Garnet chemical compositions. Image courtesy of Lina Jakaitė, Geologist, Vilnius University.
These properties are very dependent on chemistry. Pyrope, almandine, and spessartite are generally isotropic. However, the presence of the large Ca (calcium) atom in uvarovite, grossular, and andradite makes them birefringent. This may be due to strain but more probably has a structural explanation. Grossular and andradite are almost always zoned, often twinned, and distinctly not isotropic under the microscope.
Due to garnet’s tremendous range of overlapping colors, gemologists can’t identify this gem on the basis of color alone. This information is for reference only.
- Uvarovite: dark green.
- Grossular: colorless, white, gray, yellow, yellowish green, green (various shades: pale apple green, medium apple green, emerald green, dark green), brown, pink, reddish, black.
Tsavorite, a variety of grossular (5.15). Photo © Joel E. Arem, PhD, FGA. Used with permission.
- Andradite: yellow-green, green, greenish brown, orangey yellow, brown, grayish black, black. The color is related to the content of Ti and Mn. If there’s little of either element, the color is light and may resemble grossular.
- Pyrope: purplish red, pinkish red, orangey red, crimson, dark red. Note: Pure pyrope would be colorless; the red colors come from Fe + Cr.
- Almandine: deep red, brownish red, brownish black, violet red.
- Spessartine: red, reddish orange, orange, yellow-brown, reddish brown, blackish brown.
- Malaia: various shades of orange, red-orange, peach, and pink.
- Rhodolite: usually has a distinctive purplish color.
Garnets of various colors (4.56, 4.94, 19.39 // 15.4, 24.46, 9.8). Photo © Joel E. Arem, PhD, FGA. Used with permission.
Synthetic garnets have had an effect on the gem world. Before the advent of cubic zirconia (CZ) in the late 1970s, synthetic garnet was the primary diamond simulant. While they may have a smaller presence in today’s market, you’ll still find these synthetic gems.
YAG, or yttrium aluminium garnet, was the first synthetic garnet available on the jewelry market. In its pure state, YAG is colorless. However, it can be created in almost every color. The dopants used for coloring are also responsible for the wide range of refractive index and specific gravity. Colorless YAG is near the bottom of each property. YAG is not brittle and wears well. However, its dispersion is a bit low for a diamond substitute.
Manufacturers use the element yttrium, shown here in crystal form, to synthesize yttrium aluminium garnet or YAG. Photo by Hi-Res Images of Chemical Elements. Licensed under CC By 3.0.
GGG, or gadolinium gallium garnet, has a high dispersion (.038). Gadolinium and gallium are much more expensive than yttrium. However, with a dispersion close to diamond (.044), GGG makes a wonderful substitute. As with YAG, the dopants used for coloring are also responsible for the wide range of refractive index and specific gravity. Colorless GGG is near the bottom of each property. Less expensive CZ has mostly replaced GGG in jewelry today. However, these synthetics are still available in many colors. They cut beautiful gems and are a favorite of many lapidaries.
In Greek mythology, Proteus was a shape-shifting sea god. His name now means someone who easily changes their appearance or principles. So-called “Proteus garnets” are the only regularly treated garnets. A few almandine-pyrope gems from the US will change into Proteus. All the other types resist change. This treatment brings a thin layer of metals to the surface of the stone. This causes it to have a dual appearance. In reflected light, Proteus garnets have a dark gray, metallic luster, much like hematite. In transmitted light, the dark red shows through.
Garnet crystals are usually small, from microscopic up to about 6 inches in the case of grossular. Many deposits are small grains of crystals in or on their host rock. Garnets in rock, with poor external forms, may be much larger, such as the almandine from Gore Mountain, New York, which reaches a diameter of 60 cm. A few spessartites in Brazil have weighed several pounds and have retained great transparency and fine color. However, these are very rare. A typical garnet crystal is about half an inch to an inch in diameter.
Clean garnets with warm water, detergent, and a soft brush. Although relatively hard and tough, garnets can be heat sensitive. Avoid using extreme heat. See the individual entries for specific species and varieties for more recommendations. Consult our Gemstone Care Guide and Gemstone Jewelry Cleaning Guide for more information.
Ring featuring a variety of garnets. Photo © Joel E. Arem, PhD, FGA. Used with permission.