
| TANZANITE V/S FORSTERITE |
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Intorduction
Tanzanite is a zoisite mineral that is fairly new to the jewellery market. It was discovered in the 1960’s in Africa. Tanzanite is now a popular blue/purple gemstone in America and has even been placed in the same category as ruby, sapphire, emerald and opal in some markets. Its tremendous popularity, along with hand mining limitations, flooding, and government challenges, has created a shortage of this beautiful mineral.
Physical Properties
Tanzanite has a hardness of 6.5. It is blue to purple in colour, with a white streak. The luster of tanzanite is vitreous and it is transparent to translucent. It has a specific gravity of 3.2 to 3.4. Tanzanite has good one directional cleavage and uneven to conchoidal fracture. Tanzanite occurs in several habits, including prismatic, striated and columnar.
Tanzanite is trichroic or when viewd in various orientations, different colour result. The intense blue-violet colour is caused by vanadium. In one direction it is blue, in another, purple, and in a third direction it appears bronze. These colours are more intense in larger pieces of tanzanite (over 10 carats). The smaller ones are usually more pale. This property makes tanzanite easy to identify because it is a rare property.
Tanzanite looks different in different lighting situations. Sunlight usually makes it look more purple. Light bulbs and candlelight also bring out the purple and can make the grayish ones look brown. Fluorescent lights tend to bring out the blue more, as do overcast skies.
Crystallography
Tanzanite is in the orthorhombic crystal system. The crystal class is 2/m2/m2/m, while its space group is Pnmc. It has common forms of {100}, {111}, and {001}.
Chemical Properties
Tanzanite is a hydrated calcium aluminium silicate mineral with a chemical formula of Ca2Al3Si3O12(OH). It is 18.76% calcium, 12.63% aluminium, 19.71% silicon, .24% hydrogen, and 48.67% oxygen. Tanzanite has as molecular weight of 427.38 gm.
Localities
Geologically, tanzanite is found in metamorphic rocks, pegmatite rocks, and hydrothermal veins. Geographically, tanzanite is found in only one place in the world, Merelani Hills of Tanzania around Mount Kilimanjaro. Specifically, in Merereani is in the Arusha province, which is located in the Simanjiro Disrict of Northern Tanzania. It is south of the Kikuletwa River and about ten miles from the Kilimanjaro International Airport. The mines are now at a depth of 140 meters and cover an area of over 350 meters underground. Crystal quartz, pyrite, and various geodes have also been found in the mines.
History
According to legend, tanzanite was first discovered by some Masai herders when they stumbled on some blue crystals lying with some other rocks. They reported that the crystals had become blue when lightning caused a fire that swept through the area and heated the zoisite, changing the brown colour of the crystals to the wonderful blue/purple. The first person to identify this blue zoisite was George Kruchik in the early 1960’s, who was given some samples that were supposedly blue sapphire. However, Manuel D’Souza is the person credited with discovering the deposits where it is now mined. He found them while prospecting for rubies. Shortly thereafter, the Tiffany Company in New York introduced it to the world market as the gem tanzanite, named after its country of origin. In 1996 and 1997, the mining of tanzanite boomed and the market was flooded, causing the price to drop drastically. Then in 1998 terrible floods entered the mines and killed over one hundred miners. As a result, the prices rose again and remained high. Another factor in the price of tanzanite is the increased popularity in recent years.
Blue’s Brothers
The synthetic forsterite could be misrepresented – accidentally or intentionally – as tanzanite, the blue to purple gem that has taken the trade by storm in the past few years. While buying and selling a tanzanite simulant is fine – the products are beautiful and in most cases more durable than tanzanite – you should know what the simulants are so you can tell the difference. And of course you must pass this information on to your customer, preferably in writing. Failing to do so could be chalked up as fraud.
Tanzanite simulants include laboratory-grown forsterite, corundum, garnet, spinel and glass. The emergence of these simulants raises some concern because it’s easy for disreputable sellers to mix natural tanzanite parcels with look-alike lab-grown simulants without disclosing that fact. But knowing the physical and optical characteristics of tanzanite and its simulants will help you avoid making a mistake.
Synthetic Forsterite
The new laboratory-grown material, first shown in the U.S. at the 1999 Tucson gem and mineral shows, comes from the Soviet Union. Forsterite is a form of the mineral olivine (peridot) and is considered rare in nature.
Testing for Tanzanite
The quick test involves the use of an Filter, invented and developed by Hanneman Gemmological Instruments.
The synthetic forsterite that looks similar to tanzanite turns a bright green with the Aqua Filter, Synthetic Forsterite exhibits a greenish body colour, while Tanzanite shows a pinkish-orange colour.
Only Tanzanite shows both this pinkish-orange colour in the filter and the correct dichroic colours.
Other tests useful for identification of tanzanite and its simulants are :-
| Gemstone | Colour thru Filter | Dichrosim |
| Tanzanite | Pinkish-orange | Purplish-pink / Blue |
| Synthetic Forsterite | Greenish | Purplish-pink / Blue-green |
| Sapphire-Synthetic Corundum | Gray-blue | Violet-blue / Blue- green |
| Topaz | Blue-gray | Blue-rose / Coloruless |
| Aquamarine | Green | Blue / Colourless |
| Benitoite | Dispersion flashes | Blue / Colourless |
| Sodalite | Blue-gray | None |
| Spinel | Pinkish | None |
New on the market, laboratory created Forsterite is named as TANZANION. It is similar to Tanzanite both visually and in main physical properties, but is more durable in hardness and is not as fragile.
Comparison Table
| Properties | Tanzanite | Forsterite |
| S.G. | 3.38 | 3.24 |
| Hardness | 6 – 6.5 | 7.0 |
| R.I. | 1.69 – 1.70 | 1.63 – 1.69 |
| Birefringence | 0.009 | upto 0.035 |
| Chemistry : (Mg, Fe)2SiO4, Magnesium Silicate. | |
| Class : Silicates | |
| Subclass : Nesosilicates | |
| Group : Olivine | |
| Uses : As gemstones, industrial uses as refractory sands and abrasives, an ore of magnesium and as mineral specimens. |
Forsterite is named after the German naturalist, Johann Forster. It is one of two minerals of the olivine group. The other mineral is fayalite. Fayalite is the iron rich member with a pure formula of Fe2SiO4. Forsterite is the magnesium rich member with a pure formula of Mg2SiO4. The two minerals form a series were the iron and magnesium are substitutable for each other without much effect to the crystal structure. Fayalite due to its iron content has a higher index of refraction, is heavier and has a darker colour than forsterite. Otherwise they are difficult to distinguish and virtually all specimens of the two minerals contain iron and magnesium. For intermediate specimens or those difficult to differentiate as well as simplicity sake and general public recognition, they are often treated as one mineral, olivine, although it is not officially recognized as a mineral.
Forsterite is found in ultramafic igneous rocks or in marbles made from the metamorphism of dolomitic limestones. Mafic is a word that is used to define igneous rocks with a high iron and magnesium content, The “MA” is for magnesium while the “F” is for ferrum, the latin word for iron. The olivinc minerals have a high melting point and are the first minerals to crystallize from a mafic magma. Forsterite crystallizes first with fayalite crystallizing last when other minerals such as the pyroxenes are just beginning to form. This early crystallization is the reason that molten lavas will contain already crystallized grains of olivine before they are ejected from volcanoes. Some ultramafic intrusive rocks can be composed of almost all olivine and these are called dunites or peridotites. Forsterite is never found with quartz, SiOi2, as these two common minerals are unstable in each others proximity (during crystallization of course). If quartz were present, the two would react and form the mineral enstatite by the following formula:
Mg2SiO4 (forsterite) + SiO2 (quartz) = 2MgSiO3 (enstatite)
Forsterite is also found in many iron-nickel meteorites. Not just as small grains but as significantly sized crystals sometimes occupying ever 50% of the meteorites volume. Thinly cut slices of these meteorites are extremely attractive with the polished steel gray of the iron arid the embedded grains of gemmy green forsterite crystals, The effect produces the closest mineral equilalent to stained glass artwork. Some meteoritic forsterite crystals have been cut into gems.
PHYSICAL CHARACTERISTICS Colour is a light green yellow to the more common yellowish green; also known to be colourless. |
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Luster is vitreous. |
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Crystals are transparent to translucent. |
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Crystal System is orthorhombic. |
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Crystal Habits include flatten tabular to box shaped crystals, but good crystals are rare. More commonly found as grains in alluvial gravels and as granular xenoliths is magnesium rich volcanic rock. Also massive. Twinning is rare, but has produced star shaped trillings. |
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Cleavage is poor in two directions at 90 degrees, rather indistinct and rarely noticed. |
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Fracture is conchoidai. |
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Hardness is 6.5-7. |
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Specific Gravity is approximately 3,2 when pure Mg2SiO4 and rises with increasing iron content (somewhat above average for non-metallic minerals). |
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Streak is white. |
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Other Characteristics: Index of refraction is 1.64-1.71 and has double refraction. |
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Associated Minerals are diopside, spinel, plagioclase feldspars, chromite, magnetite, talc, hornblende, serpentine, iron-nickel meteorites and auguite. |
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Notable Occurrences are numerous and include the ancient source of Zagbargad (Zebirget) Island in the Red Sea off the coast of Egypt and Mogok, Myanmar (formerly known as Burma). The type locality is Mt. Vesuvius, Italy and other localities include Kohistan, Pakistan; South Africa; Ural Mountains, Russia; Norway; Sweden; France; Minas Gerais, Brazil; Eifel, Germany; Chihuahua, Mexico; Ethiopia; Mt. Franklin, Victoria, Australia; Notre-Dame-du-Laus, Quebec Canada; China and Salt Lake Crater, Oahu, Hawaii; North Carolina; Bolton, Massachusetts; Crestmore, California; New Mexico and the most productive source of peridot to date from Peridot Mesa, San Carlos Apache Reservation, Gila County, Arizona, USA. |
For further information contact
Mr. Prateek Jhaveri
Emrusa Gems & Mining Ltd.
P. O. Box : 918 Arusha, Tanzania, East Africa
E-mail : prateek_ jhaveri@yahoo.com