Tantalizing Tourmaline

rainbowoftourmaline

Tourmaline by Sandy Hoy

October's birthstones are truly spectacular. 
Along with opal, tourmaline is October's birthstone. Both of these stones are gorgeous, but tourmaline is what I want to focus on today. For too long, tourmaline has only been seen as the dull green that is widely available. This is a shame. Tourmaline comes in such a wonderful wide range of colors and with a Mohs hardness of 7 to 7.5, it is durable enough to be used in any type of jewelry.

green tourmaline

History
The first tourmaline was recorded in the 1500's in Brazil by a Spanish conquistador. The conquistador confused the vivid green of the tourmaline with that of the emerald. His mistake was not revealed until the 1800's when tourmaline was formally recognized as a distinct mineral species.
The name tourmaline comes from the word toramalli, which means “mixed gems” in Sinhalese (a language of Sri Lanka).  Dutch merchants started using the name to identify the multicolored, water-worn pebbles that miners found in the gem gravels of Ceylon (now Sri Lanka). The stones were brought to Europe in vast amounts by the Dutch East India Company as the demand for gemstones increased. As stated earlier, it was not until the 1800's when scientists were able to positively identify tourmaline as its own mineral species. As with many gemstones until the development of modern mineralogy, a stone's identity was based solely on its coloring, resulting in many stones being misidentified throughout time as ruby, sapphire, emerald, and so forth.

tourmalinefacts

One of the earliest reports of tourmaline in the United States was in California in 1892. In the late 1800s, Tiffany gemologist George F. Kunz worked to make tourmaline an American gem, praising the tourmaline deposits of Maine and California; however, it was not the American market that the tourmaline mines both in the United states and in the Himalayas ended up attracting: it was the Chinese market. 
Because the miners became so dependent on Chinese trade, when the Chinese government collapsed in 1912 the US tourmaline trade collapsed with it. The California mines stopped or moved to sporadic production. Today, mines in San Diego County such as the Stewart Lithia mine at Pala still produce a small supply of gem-quality tourmaline.
The tourmaline trade expanded again during the first half of the twentieth century, when Brazil began to mine large deposits with superb quality. In the 1950s, additional finds were uncovered in other countries around the world, including Madagascar and Afghanistan which have have produced a stunning red tourmaline.

Pink tourmaline from Pala Mountain, Stuart Mine, San Diego. (Photo: Jeff Scovil)

Pink tourmaline from Pala Mountain, Stuart Mine, San Diego. (Photo: Jeff Scovil)

Tourmaline Locations and Mining
Gem and specimen tourmaline is mined chiefly in Brazil and Africa. Additional locations include Sri Lanka, Tanzania, Nigeria, Kenya, Madagascar, Mozambique, Namibia, Afghanistan, Pakistan, and Malawi. Tourmaline is also sparsely mined in the San Diego County area of California.
Tourmaline (and some other large crystal gemstones) generally occur in an extreme form of igneous rock known as a pegmatite formation. Pegmatite is a type of igneous rock that forms during the last stages of magma cooling. Large crystals are fairly common in many types of igneous rock formations usually due to a slow rate of crystallization. With pegmatites, large crystals are attributed to low-viscosity fluids that allow the chemicals that make up a crystal to be highly mobile on an atomic level.
During the early formation of pegmatites, the magma usually contains a large amount of dissolved water and other chemicals such as chlorine, fluorine and carbon dioxide. Water is not removed during the early magma crystallization, so it becomes more concentrated as the crystallization continues. The presence of the water eventually forms large pockets in the rock. These super heated water filled pockets are also rich in the atoms of various chemicals. Within the pockets, the atoms have a much greater space to expand into than would be present elsewhere. This space combined with the extreme heat allows them to rapidly form into large crystals. The extreme conditions of crystallization in pegmatites have sometimes produced crystals that are several meters in length and weigh over one ton. 


The Colors of Tourmaline
Tourmalines make up a group of closely related mineral species that share the same crystal structure but have different chemical and physical properties. They share the elements silicon, aluminum, and boron, but contain a complex mixture of other elements such as sodium, lithium, calcium, magnesium, manganese, iron, chromium, vanadium, fluorine, and sometimes copper. It is these alterations to a tourmaline's chemical composition that directly influences its physical properties, including color. 


Many tourmaline color varieties have inspired their own trade names:

  • Rubellite is a name for pink, red, purplish red, orangy red, or brownish red tourmaline, although some in the trade argue that the term shouldn’t apply to pink tourmaline.
  • Indicolite is dark violetish blue, blue, or greenish blue tourmaline.
  • Paraíba is an intense violetish blue, greenish blue, or blue tourmaline from the state of Paraíba, Brazil.
  • Chrome tourmaline is intense green. In spite of its name, it’s colored mostly by vanadium, the same element that colors many Brazilian and African emeralds.
  • Parti-colored tourmaline displays more than one color. One of the most common combinations is green and pink, but many others are possible. Including "watermelon" and Liddicoatite. 
Liddicoatite was first recognized as a separate mineral in 1977. The mineral was named in honor of Richard T. Liddicoat (March 2, 1917 – July 23, 2002), the second president of GIA who is often referred to as the “Father of Modern Gemology.” Mo…

Liddicoatite was first recognized as a separate mineral in 1977. The mineral was named in honor of Richard T. Liddicoat (March 2, 1917 – July 23, 2002), the second president of GIA who is often referred to as the “Father of Modern Gemology.” Most liddicoatite comes from Madagascar, including this slice from the Anjanabonoina pegmatite. Coutresy Harvard Mineralogical Museum, photo by Robert Weldon/GIA

Photo courtesy of GIA

Photo courtesy of GIA

Some tourmalines have a striking cat’s-eye effect called chatoyancy. Cat’s-eye tourmalines are most often green, blue, or pink. The "eye" often has a softer and more diffused than than other stones that display the same effect. This is due to the multitude of thin, tube-like inclusions inside the stone. The inclusions are larger than the inclusions of other stones, such as a cat’s-eye chrysoberyl, so the "eye" isn’t as sharp. Like other cat’s-eye stones, tourmaline needs to be cut as a cabochon to show the effect.

What's in a name? Paraíba Tourmaline

One of the most coveted and expensive of the varieties mentioned above is Paraíba.  It is a relatively "young" gemstone in that it was not discovered until the 1980, but its vivid blues hold the attention of the entire gem world. The reason behind the vivid colors is in fact why a true Paraiba stone is so rare and special. 
Normally, iron, manganese, chrome and vanadium are the elements responsible for the beautiful colors of tourmaline. The Paraíba tourmaline is different: its color is due to copper, an element which had never before been seen in a tourmaline. The presence of copper in the stone is as much what defines the tourmaline as a Paraíba as the location from which it came. Copper in high concentrations is responsible for the coveted radiant blue, turquoise, and green hues. 

Scientists have also (relatively recently) discovered that Paraíba tourmaline may also often contain manganese as well. When both of these two elements are present they produce a variety of vivid colors such as: emerald green, turquoise to sky blue, sapphire blue, indigo, bluish-violet, and purple. They can also result in more muted pale grey to violet-blue tones. 
Because of the stone's high value in an uncut state, Paraíba tourmalines are almost always custom cut to retain as much of the stones weight as possible, however the stones are still in sizes bigger than one carat. 

The flawless 191.87 carats Paraiba tourmaline, The Guinness World Records largest, has been placed by experts in the field amongst the world’s rarest gems.

Recently scientists have discovered that Paraíba tourmaline often also contain manganese and it is the interplay between these two elements that creates the coveted colors. 

Recently scientists have discovered that Paraíba tourmaline often also contain manganese and it is the interplay between these two elements that creates the coveted colors. 

Since the late 1980s, the Paraíba area of Brazil has been a source of a strikingly colored variety of tourmaline called Paraíba tourmalines.

Since the late 1980s, the Paraíba area of Brazil has been a source of a strikingly colored variety of tourmaline called Paraíba tourmalines.

With Paraíba, the key factor is not size, but color; all factors being equal, the stone with the better color is a better choice.
During Paraíba tourmaline’s brief history, the gem has always been extremely scarce. However, new discoveries of copper-bearing tourmalines that resemble the vibrant, intense colors of the gems found in Brazil’s Paraíba region have also been found in other parts of the world. An article in the Spring 2008 issue of GIA’s Gems & Gemology scientific journal described copper-bearing gems present in Mozambique. Nigeria has become a source of these striking gems as well. With these new sources there comes the possibility that viable, commercial sources of this rare copper-bearing tourmaline might provide a larger supply of material. This brings a new problem for the niche Paraiba trade. If the stones of the same chemical composition and quality are being found outside of Paraiba does the trade name still apply? Only time and the market will tell. I personally think that the romance of a trade name should have little to do with the stone you are buying. The romance of a trade name aside, if the quality is good and the color is vibrant then that is what we should judge a stone by. 

The Lily Safra poppy flower brooch with diamond and tourmalines sold for $1,273,320 at Christie's Geneva, 5/14/2012. - © Christie's Images/The Bridgeman Art Library

The Lily Safra poppy flower brooch with diamond and tourmalines sold for $1,273,320 at Christie's Geneva, 5/14/2012. - © Christie's Images/The Bridgeman Art Library

The rainbow of colors that tourmaline has to offer the wearing is truly impressive. This stone has something to offer for everyone.  


 

 

 

 

 

 

 

 

 

 

 

 

 

 

Nicholas Varnay and K2

Nicholas Varney Blue Moonstone and Diamond Earrings: Surrounded by K2, 48 carats Blue Moonstone, 0.60 carats Diamonds. 18K yellow Gold.

Nicholas Varney Blue Moonstone and Diamond Earrings: Surrounded by K2, 48 carats Blue Moonstone, 0.60 carats Diamonds. 18K yellow Gold.

A view of K2, also known as Mount Godwin Austen, in the morning sun. With a summit elevation of 8,611 meters, K2 is the second-highest mountain in the world after Mount Everest (8,848 meters), and ahead of Kangchenjunga (8,586 meters). Image © iStoc…

A view of K2, also known as Mount Godwin Austen, in the morning sun. With a summit elevation of 8,611 meters, K2 is the second-highest mountain in the world after Mount Everest (8,848 meters), and ahead of Kangchenjunga (8,586 meters). Image © iStockphoto and PatrickPoendl.

One reason I love jewelry by Nicholas Varnay is that he isn't afraid of playing with "unconventional" stones.  One of the most interesting is K2 Granite,” also known as “K2 Jasper.”

What is K2 Granite? 

"K2 Granite," also known as "K2 Jasper," is an extremely interesting and actually slightly controversial rock and lapidary material that comes from Pakistan.

The mineral is a bright white granite that contains beautifully contrasting orbs of bright blue azurite. The azurite orbs can range from a few millimeters up to about two centimeters in diameter that can look like bright blue splashes on a rough pieces. 
K2 Jasper is the most commonly used name for marketing this material, but it is definitely not jasper. If you examine the rock closely you can see that the splotches are actually spherical. You will also see see cleavage faces of feldspar minerals and black flakes of biotite. 

The white granite is fine-grained: composed of quartz, white feldspars, and biotite. 
The azurite is a secondary material that clearly formed after all of the other minerals in the granite had solidified from the parent melt. This can be seen clearly during an examination of the azurite spheres. They are present along the mineral grain boundaries, within tiny fractures, and as a “dye” penetrating the feldspar grains.

I mentioned that this stone has been slightly controversial. When this mineral first appeared on the market the lapidary world did not believe that the blue splotches could be azurite (and to some extent this is still the case). This is because white granite and azurite rarely occur together. For many this is the first time that they have seen the two materials in such close association. 

The Controversy

For the last 3 or so years experienced mineralogists, people from Pakistan who have directly obtained K2 fron it's source, and lapidarists who have worked with K2 cutting cabochons, have had long discussions about the material; sharing observations, photomicrographs, chemical analyses, and x-ray diffraction data trying to learn more about the intrusive mineral, arriving at the conclusion that it is indeed azurite.  Some specimens were also found to have small areas that are stained green with malachite! The science of geology continues to evolve and astound! 

 

A piece of dry K2 Granite. A wet surface would increase the intensity of the blue azurite orbs. This piece is approximately 10 centimeters across, and the largest azurite orbs are about 1 centimeter across.

A piece of dry K2 Granite. A wet surface would increase the intensity of the blue azurite orbs. This piece is approximately 10 centimeters across, and the largest azurite orbs are about 1 centimeter across.

An oval cabochon cut from K2 Granite with several bright blue azurite stains. Within each stain you can see the texture of the granite and grains of black biotite. These indicate that the stain formed after the granite solidified from its parent mel…

An oval cabochon cut from K2 Granite with several bright blue azurite stains. Within each stain you can see the texture of the granite and grains of black biotite. These indicate that the stain formed after the granite solidified from its parent melt. This cabochon is about 20 x 30 millimeters in size.

Where Is K2 Found? 

As stated earlier K2 granite is named after a mountain in the Karakoram Range near the border between Pakistan and China. K2, also known as "Mount Godwin Austen," is the second highest mountain in the world. The azurite granite is found in colluvium near the base of the mountain, in a very remote area visited by very few people. 

 

 

So What About Using it in Jewelry?

K2 granite cuts, tumbles, and polishes wonderfully. Due to its high feldspar content, it can be easily cut with a lapidary saw and shapes quickly on a diamond wheel. Azurite has a Mohs hardness of 3.5 to 4, however because the azurite is more of a stain within the mother mineral, the dots have the same cutting and polishing properties as the surrounding white granite. 

As to the durability in jewelry The feldspar minerals in K2 have a hardness of about 6 on the Mohs scale, therefor they can be be scratched or show signs of wear over time if subjected to extensive use, "hard wear", or impact. K2 is therefore not a good stone for mounting in a ring or bracelet, but it is a sunning (and appropriately safe) addition to the earring that inspired this article. 

Kathleen Marino M.A, G.G., AJP, NAJA

A big thanks to geology.com for their extensive research and information on the subject. Another website to visit for more information on the mineralogical makeup of K2 or other minerals is mindat.org

 

 

Quartz Varieties

Let's talk about something that drives me nuts. Amethyst is a purple variety of quartz. It is ONLY SHADES OF PURPLE by definition. "Green amethyst" does not exist and we need to start demanding that the proper names be used.
That being said let's run through the colors and the quartz varieties:


Green quartz = prasiolite 
purple quartz = amethyst 
purple and golden quartz = bi-color quartz, ametrine,
pink quartz = pink/rose quartz
yellow quartz = citrine 
brown quartz = smoky quartz 

black quartz = black quartz
clear quartz = rock crystal quartz or clear quartz
blue quartz = blue quartz to varieties of greenish blue, and a bright clear pink (almost always synthetic and easily identified by gemologists) 

Synthetic Quartz forms in tube shapes due to the machines used to grow them  photo courtesy of WKSU news

Synthetic Quartz forms in tube shapes due to the machines used to grow them  photo courtesy of WKSU news

Also a quick word on treated and synthetic quartz. Much of the quartz (colored varieties) you see on the market are heat treated. Heat treatment can enhance or alter the color of quartz. Treatment is difficult to detect, but it is almost always assumed. 
Over the years I have also seen a lot of synthetic quartz. It is often times cut into very large stones. There are telltale indicators of synthetic quartz (that are related to the way in which it is grown) that an experienced gemologist can quickly identify.  
Synthetic quartz is just as expensive as natural quartz varieties. The is mainly due to the fact that the majority of consumers cannot tell the difference. 

As an aside, the market for synthetic quartz has always been strange to me since quartz is one of the most plentiful gemstone materials available.

How quartz is synthetic grown     photo courtesty of voguecrystals.com

How quartz is synthetic grown     photo courtesty of voguecrystals.com

Kathleen Marino M.A, G.G., AJP, NAJA

Additional photos courtesy of: Gemselect.com, gemcutter.com, dannytherockman.com, wksu news, www.voguecrystals.net,

Turquoise: The Desert Beauty

The most traditional birthstone for the month of December is Turquoise and  the zodiacal stone for Sagittarius. Opaque, varied blue colors that has been used for centuries in jewelry and in decorative ornaments.

If cold December gave you birth,
The month of snow and ice and mirth,
Place on your hand a turquoise blue;
Success will bless whate'er you do.

Turquoise is found in various locations around world that all share the same characteristics: dry, arid, barren and possessing acidic, copper-rich ground water. This ground water creeps downward it reacts with other minerals. The product of this process is the compound of hydrated copper and aluminium phosphate known as turquoise.

The deposits of turquoise usually form in iron-rich limonite or sandstone. The remnants of these host minerals (called the matrix) are what leave the veins or splotches on the turquoise. (Limonite creates the darks brown markings and the sandstone creates tan markings)
The texture of turquoise is a result of both its structure and composition. If you look at turquoise under a microscope you may see that it is actually an aggregate of microscopic crystals that form a solid mass. The closer the crystals are packed, the finer the texture and the less porous the material. Fine textured turquoise has a shiny waxy luster when it is polished, while less dense turquoise results in a duller luster.

Turquoise from Bisbee Arizona

Turquoise from Bisbee Arizona

The porosity also affects the stones' durability with the less porous turquoise possessing less toughness. Because of the decreased visual appeal and the lesser amount of durability more porous turquoise is often treated to make it smoother, shinier, and more marketable.

turquoise

                                                                                                                                                                                  Most people will be familiar with vein like black matrix running through the vibrant blues or greens; however, the most expensive and prized turquoise has no matrix showing. The second most valuable is a thin web like matrix that is evenly distributed throughout the stone.This really is personal preference, and some turquoise lovers may find imperfections part of the charm.

Turquoise is very soft, ranking a 5-6 on the Mohs hardness scale. This makes the stone ideal for carving and artists throughout history in Europe, Asia, the Middle East and  the Americas have utilized it as a medium for both jewelry and art objects.

Turquoise has a long and varied history (that continues to this day) of being used as talismans, amulets, or religious artifacts as it has been attributed to have special power and meaning to various cultures. The ancient Egyptians, Meso-Americans, Native Americans and Tibetans have believed in the special powers of turquoise for centuries. Some believed that turquoise can protect its wearer from harm, others thought that it brought good luck or longevity, and some uses and meaning have been lost to history.

                  Egyptian middle Kingdom faiance hippo                                       The MET Mu…

                  Egyptian middle Kingdom faiance hippo
                                       The MET Museum

The high value placed on fine turquoise caused many imitations to be made. The first of which dates back to ancient Egypt: a glazed earthenware material called faience. Later glass, and enamel were used. In modern times plastic, porcelain, composites of minerals were used. In 1972 the closest “synthetic” turquoise was produced by Pierre Gilson. I put synthetic in quotes since it is actually called a simulant owing to its chemical composition differing from actual turquoise due to a bonding agent. The simulated turquoise is available in both fine and spiderwebbed varieties.

The most common natural stone imitators of turquoise that might be encountered are dyed howlite and magnesite. These stones are both white in their natural state and contain black veining.

All of these imitators are fairly easy to identify by a  trained gemologist and many can be identified by the general consumer as well.

Basics:
Chemical Formula: CuAl6(PO4)4(OH)8•4H2O Copper containing basic aluminium phosphate
Hardness: 5 to 6 on the Mohs scale
Formation:Turquoise occurs as botyroidal (grape-like) masses or nodules in fissures.
Found in: Currently the finest quality turquoise is found in Northeast Iran. Major turquoise deposits are also found in Afghanistan, Argentina, Australia, Brazil, China, Israel, Mexico, Tanzania and the USA.