November 2016

Topaz in matrix (Photo GIA)


The Colorful World of Topaz

I have always thought it was a shame that the general public has been forced into the misconception that topaz is merely and inexpensive blue gem. Incidentally the blue color is hardly ever natural: It’s almost always caused by treatment. Topaz has a far broader and more colorful story to tell gemstone lovers. 

Topaz is allochromatic. This means that the color you see is caused by an elemental impurity or defect in its crystal structure rather than by an element of its basic chemical composition. For example, the presence of the element chromium causes natural pink, red, and violet-to-purple colors in topaz. Imperfections at the atomic level in topaz crystal structure can cause yellow, brown, and blue color. Brown is a common topaz color, and the gem is sometimes mistakenly called “smoky quartz.”

The 97.45-carat Blaze Imperial Topaz is in the collection of the Field Museum of Natural History. - (Photo: "Gems and Gemstones: Timeless Natural Beauty of the Mineral World" by Grande & Augustyn, U of Chicago Press.)

Topaz actually has an exceptionally wide color range that, besides brown, includes various tones and saturations of blue, green, yellow, orange, red, pink, and purple. Colorless topaz is plentiful, and (as was mentioned earlier) is often treated to give it a blue color.

The color varieties are often identified simply by hue name—blue topaz, pink topaz, and so forth—but there are also a couple of special trade names. Imperial topaz is a medium reddish orange to orange-red. This is one of the gem’s most expensive colors. Sherry topaz—named after the sherry wine—is a yellowish brown or brownish yellow to orange. You may hear stones in this color range are referred to as "precious topaz". This term is used to distinguish them from less expensive citrine (yellow quartz) and smoky quartz.

 

Topaz crystals are typically elongated, with grooves parallel to their lengths. For this reason, they're commonly cut into long oval or pear shapes. These crystals show orange, pink, and brown colors. - Eric Welch/GIA


What is Imperial Topaz?

Red is one of the most prized and rare topaz colors. Red represents less than one-half of 1 percent of facet-grade material found. The color known in the gem the trade as "imperial topaz" is even more highly prized and rare. They color is a bit elusive and subjective; however, many dealers insist that a stone must show a reddish pleochroic color to be called imperial topaz. The reddish pleochroic color often appears at the ends of fashioned gems—like pears and ovals—that have an otherwise yellow-to-orange bodycolor. This look is illustrated in the images below. 
The name for "imperial topaz" originated in nineteenth-century Russia. At the time, the Ural Mountains were topaz’s leading source, and the pink gemstone mined there was named to honor the Russian czar. Ownership of the gem was restricted to the royal family.

This untreated 45-carat imperial topaz displays an attractive reddish peach color. (Photo: Constantin Wild, Idar-Oberstein)

Spectacular prize-winning, orangy-red, flame-shaped Imperial Topaz gem. (Photo: Gem courtesy of John Dyer & Co.)


The Württemberg Pink Topaz Tiara

The Württemberg Pink Topaz Tiara features pink topaz stones 

This tiara is part of an extravagant parure which includes, the tiara, two bracelets, a pair of earrings, and a devant de corsage (large brooch).  The set features a series of large and small pink topaz stones, surrounded by diamonds, mounted in gold and silver.

Princess Marie in the Topaz Parure

All of the pieces feature diamonds and striking pink topaz. The topaz stones are believed to be sourced from Russia.
The parure is linked to Princess Marie of Waldeck and Pyrmont (1857-1882), who married Prince William of Württemberg (later King William II) in 1877. Marie died just five years later following complications during the birth of her third child, a stillborn daughter.  Her pink topaz jewels are no longer with the Württemberg family and were last associated with the Faerber Collection.

 

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Gemology 101

Allochromatic: When color is caused by impurity elements or defects in its crystal structure rather than by an element of its basic chemical composition.
Idiochromatic: An idiochromatic gem is one where the color is not due to impurities, but where the coloring element is an essential part of its chemical formula. An example of an idiochromatic gemstone is peridot, because iron is part of its makeup; no iron, no peridot. 
Pleochroic: Pleochroism is when a gemstone shows different colors in different crystal directions. 

Pleochroism in a tourmaline cut with the c-axis parallel to the table, as seen with the unaided eye through the side (left), crown (center), and end (right). (Photos: Wimon Manorotkul and Mia Dixon.)


What You Might Have Missed

October 2016

october

American Contra Luz Opal from Oregon, Sold by Bonhams Auction House

Opal

Opal is formed in dry areas such as Australia’s semi-desert “outback.” Seasonal rainwater drenches the dry regions and showers soak deep into ancient underground rock, carrying dissolved silica (a compound of silicon and oxygen) downward, forming deposits in cracks between rocks. During dry seasons much of the water evaporates, leaving the silica deposits underground in the cracks and fissures of sedimentary rock.

Depending on the conditions in which it formed, opal may be many colors. Precious opal ranges from clear through white, gray, red, orange, yellow, green, blue, magenta, rose, pink, slate, olive, brown, and black. Of these, black opals are considered the most rare while white and greens are the most common. 

As with their color opals vary in optical density from opaque to semitransparent, and there are two broad classes of opal: precious and common. Precious opal displays play-of-color while common opal does not.

Play-of-color occurs in precious opal is due to the way in which silica is arranged on a sub-microscopic level. Opal is made up of sub-microscopic silica spheres that arranged in a grid-like pattern (think of it like a box of ping pong balls). This arrangement causes light to bend (diffract). As the light bends it breaks apart into spectral colors (all the colors of the rainbow) producing an incredible display of color.  The color that can be seen varies with sphere size. According to GIA "spheres that are approximately 0.1 micron (one ten-millionth of a meter) in diameter produce violet. Spheres about 0.2 microns in size produce red.  Sizes in between produce the remaining rainbow colors".

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Opalized Fossils

OpaliZed freshwater mussell shells 110 million years old

What are Opalized Fossils?

Opal usually forms within fissures in rock layers, but opal can also form in other materials. If a cavity has formed because a bone, shell or pine-cone was buried in the sand or clay that later became the rock, opal may form in these cavities. 
One of the richest sources of opalized fossils is Lightning Ridge in northwestern New South Wales. These fascinating fossils transport us back in time approximately 110 million years! The fossils of dinosaurs, marine reptiles, fish, early mammals, mollusks, and plants give us a window into our planet's history. 

There are two kinds of opalized fossils:

Type 1. In this type the internal details are not preserved. The water and silica solution fills an empty space left by a shell, bone, etc. that has disintegrated away and then hardens to form an opalized cast of the original object. The opal inside doesn’t record any of the creature’s internal structure. Most opalized shell fossils are this type of ‘jelly mold’ fossils. 

Type 2. In this type internal details preserved: If the buried organic material hasn’t rotted away and a silica solution soaks into it, when the silica hardens it may form an opal replica of the internal structure of the object. This happens most often with with wood or bone.

OpaliZed theropod dinosaur tooth. Lightning Ridge, New South Wales.

OpaliZed Fossil Wood from Queensland Australia


The Virgin Rainbow

THOUGH superficially Belemnites resembled squid, they are distinct from modern squid for several reasons. they possess hard internal shells/skeletons composed of calcium carbonate and also lacked the pair of specialized hunting tentacles POSSESSED by modern cuttlefish and squid. belemnites instead hunted with ten arms covered in tiny hooks. (Artist's depiction of a belemnite school)

The Virgin Rainbow, it was discovered in the opal fields of Coober Pedy by opal miner John Dunstan in 2003. 
It's actually an opalized fossil, from an extinct cephalopod called belemnitida that existed during the Mesozoic era. During that time, much of South Australia was under a vast sea that was filled with prehistoric aquatic life. When these creatures died they sank to the bottom of the sea and were buried by sediment.

Over the millennia the sea eventually dried up and the land turned into a desert. The acidity levels in the shallow top layer of the sandstone increased causing the release of silica from weathering sandstone. Groundwater then carried it down to the layer of clay beneath, where bones and pockets left by disintegrated bones lay buried.

Further weathering lowered the acidity levels allowing the silica gel to harden into opals in the pockets and impressions left by decayed animal material to create a replica of the internal structure (see a description of opalized fossil types above).

The famous Australian opal fields of Coober Pedy are located in this prehistoric sea region. No other environment in the world is known to have undergone this same process, which very well may be why over 90 percent of the world's opals come from South Australia.

Artist rendering of a Plesiosaur next to the Addyman Plesiosaur

Opalized fossils in this region are not uncommon. The South Australian Museum is home to a spectacular (almost complete) opalised skeleton of a six-metre (20-foot) plesiosaur known as the Addyman Plesiosaur, although you have to look closely to see its opalescent sheen. This is not the case with the Virgin Rainbow.

The Virgin Rainbow opaliZed fossil of an extinct cephalopod called belemnitida that existed during the Mesozoic era.

"You'll never see another piece like that one, it's so special. That opal actually glows in the dark -- the darker the light, the more colour comes out of it, it's unbelievable," said Dunstan.

"I've done a lot of cutting and polishing [of opals], I've been doing it for 50 years, but when you compare it to the other pieces that claim to be the best ever, this one just killed it." 

The Virgin Rainbow is considered to be the finest opal ever unearthed and is worth more than $1 million. (In case you were wondering the Virgin Rainbow isn't even the most valuable opal in the world! A massive, 3.45-kilogram (7.6-pound) stone named the Olympic Australis opal, excavated in the Coober Pedy in 1956 gets that honor. In 2005, the Olympic Australis was valued at $2.5 million.)

Both the Addyman Plesiosaur and the Virgin Rainbow are currently on display among a dazzling collection of opals at the South Australia Museum in an exhibition, called "Opals". The exhibition began in September 25, 2015 and will run until February 14, 2016. 

"From jewellery to fossils to specimens embedded in rock, visitors will be treated to a spectacle of unmatched colour and beauty. This is an exhibition literally millions of years in the making because these opals were formed back when dinosaurs walked the earth and central Australia was an inland sea," - Museum Director Brian Oldman.

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Gemology 101


Aboriginal Origins of Opal

"The Path of Enlightenment" necklace contains 180 magnificent opals from Lightning Ridge, Australia, a famous opal producing area. - Courtesy Cody Opal

We Came From the Land  
This aboriginal story teaches how areas around the Flinders Ranges were created and the origins of opal. This is a Wirangu story from near Ceduna on the west coast of South Australia as told by M. Miller and W.J. Miller.

A long long time ago, a huge meteorite hurtled towards the earth from the northward sky, and smashed into the ground near Eucla. Because it was so big, a dent appeared in the crust of the earth and the meteorite bounced high into the air and out into the Great Australian Bight where it landed with an enormous sizzling splash. It was hot from its trip through space so it gave off a great deal of steam and gas as it sank through the waves. But this was no ordinary meteorite. It fact, it was the spirit Tjugud.
In the deep water near by, the spirit woman Tjuguda lay asleep. All the noise around her woke her up and she was very angry. She bellowed and the elements roared with her. The wind blew, the rain pelted from the sky and the dust swirled.
From the joining of the two spirits, the Tjugud and Tjuguda, a man was born, but he was no ordinary man, he was of enormous proportions. He rose from the deep water of the Bight to swim through the maze of limestone caves which run through the earth and into the sea. Then, he emerged from the ground through the cave of the Nullabor.
This was the birth of the Wirangu man, a coastal dweller. Wirangu walked towards the east, taking huge steps in keeping with the stature of the man. Each time he stepped, the ground shook and a dent appeared in the earth. These would later fill with water and are the rock holes which can still be seen today. You can clearly trace the journey of this man.
When he reached Coober Pedy, he was very hungry so he found some food and then lit a fire. The fire he built was so fierce it burned with an enormous amount of heat. A lot of water from the body of the man dropped into the ground and was captured by the stones which held a lot of water anyway. The beautiful colours from the raging fire went down into these stones, changing the water into a magnificent display of color. This is the colour of the opal and can be found in the stones still.

(Education Department of South Australia 1992: 32-33)

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What You Might Have Missed