Astutely observed by Mab Wilson, author of Gems:
|“||Most of us, having been brainwashed by the dark and depressing parures of the turn of the century, forget the many beautiful colors garnets can have. Badly cut, a garnet can indeed be a melancholy object, lugubriously red and usually in a brown study; but a clear and well-cut garnet can be bright as a zinnia, as dark as a bottle of red ink, as green as an emerald or the very green of a dew-moistened leaf of the lily of the valley.||”|
Garnets, with their wide range of colors and varieties, have long been an important gem material throughout history with research dating their use back to the earliest known civilisations.
The name garnet is derived from the Latin word granatas, meaning grain or seed. Historically the red varieties of this gemstone, which resemble the seeds of a pomegranate in color, were referred to as garnets. The term garnet has come to refer to the whole family of minerals that crystallize in the cubic system and share the same chemical blueprint. The elements used to fill that blueprint place a gem garnet into one or more of the following:
It would have been easy if nature presented us with pure family members but, unfortunately for those trying to classify garnets, this is not the case. The family members listed above represent "end members" within the garnet group. In other words, their composition is an ideal, theoretical one. In reality, all the garnets we use as gem materials are a mix of two or more end members in various ratios. Some of the magnesium which makes a pyrope a pyrope can be replaced by iron, or some of the iron that makes an almandine an almandine is replaced by manganese. In gemology this 'mixing of end members' is called isomorphous replacement.
The composition of a garnet determines certain measurable characteristics of the stone such as refractive index and specific gravity. It can also influence the color of the stone, which is why garnets come in many colors and shades. The confusion which occurs from these mixed garnets, together with marketing strategies, have caused an array of trade names to be invented for various garnets. While it is scientifically correct to call the the green garnet found in Kenya a green grossular, the gem trade insists on (erroneously) calling it Tsavorite. It sells better that way. Some names are relatively new and are still being contested, others have been in use so long that they have gotten a firm grounding in literature and have been adopted by gemologists. It is important to remember that, at the end of the day, all garnets are a mix of two or more of the end members mentioned above.
Below is a diagram of trade names (developed by Dr. W. Wm. Hanneman) placed into context using their actual composition:
Garnets have been used, wherever they occur, for as long as mankind can remember. From predynastic Egypt to the discovery and hype of Fanta orange garnets in Tanzania in 2007, garnets have never ceased to capture our attention. The Roman writer Pliny mentions gemstones called carbuncles, some of which are thought to be garnets. The red family member, almandine, was a very popular gemstone with the Germanic tribes that inhabited northern Europe during Roman times. They were used for cloisonné inlay work of which items found at Sutton Hoo are a great example.
During the Victorian era garnets were extremely fashionable; rose cut garnets from the Czech Republic often covered entire jewelry items. These garnets are better known as Bohemian Garnets after the area they were mined: Bohemia.
Andradite was discovered in the Ural Mountains of Russia circa 1853. This distinctively bright green garnet was given the name demantoid in 1878. It quickly became a "hot" gemstone punctuating 'turn of the century' jewelry.
In the last quarter of the 20th century various additional garnet varieties have been found in Africa.
|Treatments:||Usually Not Treated|
|Country of Origin:||Worldwide|
|Warm Soapy Water:||Safe|