August 2005 Newsletter

I have just returned from Ste Marie aux Mines in France. We visited the mineral show and I have included a report of our visit in this newsletter. I will add photos to the photogallery. I have listed some specimens on my website from the show. The rest of our purchases are at our store in Hartbeespoort. We bought some fantastic items at the show. Fossils, unique jewelry and great specimens.

I also have more on the Kalahari manganese field and its geology, next month we will have more on the minerals from this locality

I also wrote a thought provoking article on the situation at Kuruman. I hope to raise some debate with this article. Not everybody understands what we see in a rock. For these people it just remains rocks and nothing more.

The sale was a great success at our store. We sold some boxes filled with minerals for less than $ 2 per box. People bought hundreds of boxes. I hope you all enjoyed it.


    This month we cover the following

  • Ste Marie aux Mines 2005, show report.

  • What is happening at Kuruman?

  • Mineral of the month :Emerald

  • The Kalahari Manganese fields

    Be blessed as you read this newsletter.

    Gerdus

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Ste Marie Aux Mines 2005

We arrived in France on the Monday around midday with Emirates air via Dubai. The yourney gave me enough time to get familiar with my new camera. You will see an improvement in my pictures.

In the afternoon we just strolled the streets of Paris and soaked up the scenery. We even took a boat trip down the Seine. We then strolled back to our hotel after visiting an Italian restaurant.

The next morning we took a bus to go and see the George Pompidou center. We landed up at Place George Pompidou on the other side of town. Geran and me had a good laugh and then we headed back to our hotel to catch the train to Ste Die. We did not know that traffic practically comes to a standstill on the lunchhour. And we took a bus. Learn a lesson here. Always take the metro. We missed our train and thus we started with our adventure. This meant that we had to take another train. Well France is a civilized place and they did not penalize us. We arrived in Ste die at sunset and decided to get to Ste Marie in the morning because we did not know what to expect in Ste Marie.

That evening they had a music evening in France, Everybody that could play a musical instrument was out on the streets. And we had fun, lots of fun. American line dancing, folk music, string quartets and rock bands competed for peoples attention. WOW!! Well done Europe!!

The next morning we got a lift with our new French friend Piot to Ste Marie aux Mines.

Ste Marie aux Mines is a picturesque town situated in the Alsace region of France. This area borders Switzerland and Germany. A lot of detail can be gleaned from the official website of the show and great pictures are also to be found there. www.euromineral.fr

This is my first time to this great show. This show is regarded as one of the big three international shows. Tucson, Munchen and Ste Marie Aux Mines. It is the flagship of the French mineral shows.

Some interesting things I discovered about the town made me appreciate it so much more. It used to be a mining town and then a center for textiles. But it has since fallen into slight disrepair because of a slow economy in the area and collapse of the textile industry in Europe. This show is the biggest event in the area during the year.  We had to stay 25 km outside of town whereas I could see dozens of empty buildings in town, I guess that one event a year does not justify the cost of renovation.I liked the old look of the town with unpainted buildings. So much character was to be seen all over.

Luckily the show is going to stay in Ste Marie for the next year.

We were fortunate to be there on the set-up day. It was fascinating to see how the guys cart in these huge geodes from places such as Brazil.

My son was with me and we just strolled through the show looking at what was available. The first items we saw were stalls from China. Here we communicated by calculator. I bought some great stibnite and fluorite on the first day. I carted a heavy fluorite from Riemvasmaak with me for a client and thought this one inferior to the fluorites from China. When I first saw the Chinese fluorites I was highly impressed with the color and size of the octahedral crystals. The crystals had such fine form. Upon my return my beautiful fluorites turned out to be ugly ducklings. That is after the oil has dried. I knew they were oiled but I did not know that the change would be so remarkable once they dry. Can someone give some advice here. The most expensive one also came in pieces out of the box they packed it in. The problem now is that I only have myself to blame. I read other show reports but only read it with passing interest. My Riemvasmaak fluorite turned out to be a gem amongst these treated Chinese fluorites.

The show appears to be small at first but after a few days we still discovered new areas that we have not yet seen. It is like a labyrinth. There is so much to buy. I was mostly buying for my store. Choices, choices. I was not buying and looking at the show from a purely collecting viewpoint. So if I fail to tell you about what is new you must excuse my ignorance. To learn everything about minerals takes a lifetime and to keep a pulse on what is new in the mineral world takes even greater commitment. It is such a great hobby. You can collect a lifetime and still learn more and more as you go along and discover new mineral producing areas. Every locality has it's own appeal. And it is often unfair to compare one locality to another.

I live at one of the worlds most unique localities, Kalahari Manganese Field. It might not be the most prolific but it sure brings forth great rare minerals every often. I took some aesthetic Kalahari minerals and Namibia minerals along and the ones that sold best were the Kalahari minerals. The Brucite specimens were well received. The sturmanites were also well accepted. You learn every time that you expose yourself to the sellers market. You see what people look at and sometime you might value something highly but nobody looks at it. Well it might just be the type of buyers that looked at the goods as well. We are the sum total of what we have become up to now. So your knowledge and appreciation for minerals is directly related to the sum total of exposure that you have had to the hobby.

The Chinese had some interesting specimens such as realgar and orpiment. I looked at several specimens but none came close to satisfying my strict criteria for aesthetics.

I made friends with some Bulgarian dealers who impressed me with the quality of their minerals. I have listed a few of these over the last couple of days. I was fortunate to buy these specimens on the set-up day so I guess I was the first to take a look at it. The paragenesis is fascinating. The specimens consist of metals in shiny colors and this really appealed to me. I was told by Alexander Dikov that the silver color is caused by the high content of actual silver in the galena. Well maybe someone out there have another theory.

It is winter in the southern hemisphere and we moved North to where it was summertime. So the temperature in France was a surprise. Temperatures were well into the 30's. It was hot, hot, hot especially in the theater balcony and the tents. Heat just builds up under the lights.

The theater housed the high-end dealers. Always a joy to see, but as a dealer and shopkeeperI found the prices a tad high. But some very good rhodochrosites from Home Sweet mine was to be seen in one of the cases. There were a lot of Pakistan aquamarine. But I found many to be a bit pale for my liking. They lacked 'oomph'. The silver on matrix from Spain was interesting.

We soon found our favorite places to have lunch at. The French make such great food. And the beer was not to bad either.(We preferred the German beers)

We slept outside of town in the direction of Preferred Bonhomme. A house can be had for about Euro 100 per day. What a deal!! And several people can share such a house. We shared with the group from Mikon. They treated us for several days. We had lifts in to town and ate with the company several times. It was great to stay with people who were familiar with the show and the protocol of the show.

In general people were rather laid back. Some would sit in their booths without a shirt and drink beer to replenish lost moisture, remember that I told you that it was hot. We liked the musicians who walked through the show and who played music to us. There were music from everywhere. This just helped to add to the already pleasant atmosphere.

Most mineral producing areas were well represented. Romania had good representation with their stibnite on the balcony of the theater. I bought a stunning calcite cast with pyrite there and one of their stibnites or antimony as it was labeled. India had some representation but it saddened me that such great minerals were overexposed to the market and in the process it might have lost some of it's appeal. I bought one flat of very good okenites. I love the cottonball spheres.

The Chinese were riding the wave but I am afraid that too much of their minerals from one source will also cause the demise of the popularity of certain of their minerals. Maybe I can have some feedback from other collectors and dealers on this.

We always have a fight with quality and prices. When something is very good and colorful it can ask for high prices. But the high prices makes these minerals a sort of an elitist item. If you have the money you can buy the minerals. And high prices are then a mark of the esteem that you hold the item in. Well we all have to make money to stay in this business. But this spiral often scares me. I also buy higher priced items because we have raised our standards lately but we have found that these super minerals are often slow sellers on a website because they have to be seen to be bought. Just imagine that you buy minerals from a locality every day and along comes one that is obviously superior to all the others. The seller knows it is superior and if you pay too little he will not be back with this class of items. So you just have to pay to have the best. So I guess this is where shows become essential to sell your top items. But at a show you are just one of many who need to make a sale.

Our trip was concluded with another three days in Paris. We saw great art, walked the streets, had great French food and went shopping for gifts. Well let me not bore you with all the details.

I will definitely be back next year. It takes you at least 3 times to a locality before you get the hang of it and knows where the best deals are to be found. I have included some pictures and hope that these do not make the e-mail too big.


    What is happening at Kuruman?

      Not much has surfaced recently. This is due to the following factor. The mine has been very serious in blocking any flow of minerals to the outside market.This is not good news to the mineral community at large. The Kalahari manganese fields has always been known for the great variety of minerals from here. The minerals should be the showcase of everything fantastic from Africa. We should be proud of the fact that we can offer these great minerals to discerning collectors worldwide. We should encourage the collecting and marketing of this great resource. But we block the flow of such minerals. The mine should have a policy of collecting and careful marketing.

      I welcome any cooperation of the mines to help with collecting and the marketing of this resource. It is not just a resource, it adds value to peoples lives. It teaches kids an appreciation for nature. It should make our country proud that we have such great minerals.

      And now they block the flow? I do not understand this. This can only result in dishonesty and destruction of the minerals. Let me paint a picture here. A pocket is found by a miner. He realizes that the pocket will be closed up and he then starts to collect whatever he can find in as short a time as he can. This results in poor collecting practises and destruction of the pocket. They should rather have an incentive system where the miners are rewarded for finding a pocket of minerals. I have often been asked why our minerals reach the market in such a poor damaged state. Well this is because nobody at the mine realizes the value to the collector and I am not talking of financial value here. The value is measured in the enjoyment of the minerals by themselves.

      This destruction has also lead to the high prices of the minerals. Only a handful of fine specimens see the light and these are then treated as 'gold' They are regarded in such high esteem by the sellers that the prices can become inflated.

      I realized that we have a lot to learn on my recent trip to France. I often wished that I could take more people to such shows so that they can learn how the pricing structure works and learn of the high standards that collectors set for minerals.

      I can get minerals from anywhere. I can take a drive up to Namibia or Malawi or even the DRC and get minerals from any number of places. I fly to new localities every month.  My business is not reliant on minerals from this locality  but Kuruman has always add value to my life because of the unique suite of minerals found here. I can say that I am crazy about the minerals of the Kalahari

      I know that this article can lead to some serious debates. I also know that my site is followed by collectors all over and that some people even use it as a base for information on what is happening here. I hope that I can get some feedback from the local mines and that we can start working together to preserve this great mineral heritage. The sad thing is that it takes the next generation to look back in hindsite and say that we should have done more. I ask that we do something now so that we do not have to regret it later.

The Kalahari Manganese fields.

We are grateful to Christian Weise for permitting the translation of this article from the original Lapis German text.


Geology of the Kalahari manganese field

Previous Studies

Several systematic geological and mineralogical studies have been conducted to obtain a detailed understanding of the mineralogy of the different types of manganese ores present in the Kalahari manganese field. Cairncross, Beukes, and Gutzmer (1997) recently summarized the results of these systematic studies. It is not the aim of this article to present a detailed review of the rather complex mineralogy of the manganese ores; more than 135 minerals are known. Instead, the focus is on selected minerals that can be regarded as the "classics," those that have established the Kalahari manganese field as one of the classic mineral specimen localities worldwide (Cairncross and Gutzmer 2000). However, mention will be made of associated species and of more recent discoveries that have not previously been covered in the literature.

General Geology, Mineralogy, and Ore Formation

The manganese ores of the Kalahari manganese field occur in three seams extending over 17 kilometers east-west and 45 kilometers in a north-south direction. These were delineated by exploration drilling and mining over an area of approximately 1,100 square kilometers. The lowermost of the three seams is by far the thickest; it hosts the largest part of the ore reserves and is currently the only seam mined. It attains thicknesses of up to 49 meters in the south, near Mamatwan, decreasing systematically to a thickness of 5 meters in the northernmost part of the field. The middle seam is laterally discontinuous and never exceeds 2 meters in thickness. The uppermost of the three seams is again continuous but also of only minor economic importance, as it does not exceed 5 meters in thickness.

Each of the manganese ore seams is located in the center of a well-defined cycle of chemical sedimentary rocks. These cycles consist of banded iron-stone, overlain by rhodochrosite-rich hematite lutite and carbonate-rich manganese lutite (i.e., the manganese ore). This succession of iron- and manganese-rich chemical sedimentary rocks is up to 100 meters thick and is known as the Hotazel Formation (see fig. 2). The Hotazel Formation grades vertically into stromatolitic dolomites and limestones of the Mooidraai Formation and rests conformably on basaltic andesites of the Ongeluk Formation. This triad constitutes the youngest part of the Transvaal Supergroup in the Northern Cape region, a several-kilometer-thick succession of chemical and elastic sedimentary rocks with minor volcanic rocks that formed 2.6-2.1 billion years ago. The Hotazel Formation and overlying dolomites were deposited about 2.25 billion years ago in a shallow shelf environment or a largely isolated marine basin bordering a large continental land-mass called the Kaapvaal Craton. The cyclical deposition of iron- and manganese-rich rocks is tentatively explained as a consequence of repeatedly rising and falling sea level and associated systematic variations in the physicochemical conditions in the depositional environment. Both iron and manganese were precipitated from the sea water and submarine hydrothermal exhalations, along ancient midoceanic ridges, that are widely regarded as the ultimate source for the metals.

[FIGURE 2 OMITTED]

The carbonate-rich manganese lutite contains 20-40 weight percent manganese and accounts for approximately 97 percent of the total manganese resource of the Kalahari manganese field. This so-called Mamatwan-type of manganese ore is of little interest to the mineral collector, as it is typically microcrystalline and composed of very few intimately intergrown minerals, including braunite, hematite, hausmannite, jacobsite, kutnohorite, and Mn-calcite.

Higher-grade ore, containing 45-70 weight percent manganese, formed by hydrothermal or supergene processes that affected and altered the low-grade Mamatwan-type ore. Surficial weathering processes are invoked to explain the observed enrichment of the manganese ores along the suboutcrop of the Hotazel Formation against the overlying Late Tertiary and Quaternary calcretes and windblown sands of the Kalahari Formation. The exposure of the low-grade manganese ores to oxygenated groundwater results in the decomposition of manganese-bearing carbonates and leaching of carbon dioxide, calcium, and magnesium. Furthermore, braunite and kutnohorite are oxidized to form a microcrystalline mixture of [Mn.sup.4+] oxyhydroxides, such as todorokite, manjiroite, cryptomelane, and pyrolusite. This type of super-gene-enriched ore is rather scarce and constitutes less than 1 percent of the total ore resource. Being exceedingly fine grained, this ore type also yields few collectible mineral species. However, the circulation of groundwater through fractures in the manganese orebodies in geologically recent times may well be responsible for the formation of well-known minerals: for example, the scalenohedral rhodochrosite crystals perched on coarsely crystalline manganite from Hotazel and N'Chwaning I. and the asbestiform fibers of manjiroite and todorokite to 7 cm long at the old Smartt mine in the southern part of the Kalahari manganese field.

Economically important volumes of high-grade manganese ores (3 percent of the total ore resource) are restricted to the northernmost part of the Kalahari manganese field, where normal faults have displaced a west-verging thrust system and duplicated the Hotazel Formation. Hydrothermal enrichment took place when hot, water-rich fluids, with temperatures ranging from 100 [degrees] C to 250 [degrees] C, percolated along the normal faults during the so-called Namaqua-Orogeny, some 1.1 billion years ago. As these hydrothermal fluids reached the Hotazel Formation, they leached calcium, magnesium, and carbon dioxide, as well as some silicon dioxide from the low-grade ore, leaving a coarse-crystalline, porous, and massively textured residuum of recrystallized hematite and manganese oxides, such as hausmannite, braunite, and bixbyite. It is this high-grade ore, which is commonly referred to as the Wessels-type ore, that is the most sought-after resource of the Kalahari manganese field.

The Wessels-type ore is not only of greatest economic importance, but it also constitutes the host rock for virtually the entire suite of mineral specimens found in the Kalahari manganese field: more than 110 minerals are currently known to occur in this ore type. These minerals owe their origin to the complex mineralogical and geochemical changes that took place during the transformation of carbonate-rich microcrystalline Mamatwan-type ore to carbornate-poor coarse-grained Wessels-type ore. Several favorable factors contributed to the resulting mineralogical complexity, including:

* Water-rich hydrothermal fluids reacted with a rock type of unusual composition (manganese- and carbonate-rich). Dissolution of the manganese-rich carbonates rendered the pH of these fluids weakly alkaline, which is unusual for hydrothermal fluids.

* The open hydrothermal alteration system permitted the escape of gaseous-carbon dioxide.

* Dissolution of carbonates present in the Mamatwan-type ore led to a rapid porosity increase that, in turn, furthered the reaction progress between fluid and ore.

* Several chemical elements--such as calcium and magnesium but also boron--were saturated in the hydrothermal fluids as the alteration process progressed. Cooling of these fluids then led to mineral precipitation.

* The prevailing oxidation potential in the hydrothermal alteration system supported the stability of [Fe.sup.3+], [Mn.sup.2+], as well as [Mn.sup.3+]-bearing minerals.

The hydrothermal minerals may thus be regarded as the product of leaching and redistribution of elements that were present in the low-grade Mamatwan-type ore. The hydrothermal fluid introduced only small amounts of water and alkali elements (such as sodium and potassium).

The mineral assemblages of the Wessels-type ore may be subdivided into three large paragenetic groups: (1) an early stage of alteration, (2) the main phase of alteration, and (3) minerals that formed during the waning stages of alteration. Some minerals, such as hematite, hausmannite, and andradite, formed during all three stages, but most are found only in very specific associations, The early phase of alteration is marked by the formation of fine-grained skarnlike bodies that often preserve the sedimentary textures of the Mamatwan-type protore. Dense, purple-colored masses of sugilite, which is traded as a semiprecious stone, are probably the most well-known product of this early stage of alteration. Sugilite is often closely associated with alkali-bearing calcium and calcium-manganese silicates. These include pectolite, wollastonite, and johannsenite but also several of the minerals that are unique to the Kalahari manganese field, such as effenbergerite, wesselsite, kornite, and hennomartinite.

Minerals attributed to the main stage of hydrothermal alteration are typically found as constituents of the coarse-crystalline Wessels-type. They may also, however, occur in well-developed idiomorphic crystals that line dissolution rugs in the orebody. The best examples are undoubtedly the attractive assemblages of large crystals of hausmannite and hematite, closely associated with andradite and clinochlore.

Most of the mineral diversity of the Wessels-type ore field can, however, be attributed to the late, waning phase of hydrothermal alteration. Many of the rare minerals that occur in unusually large and well-developed crystals in the Kalahari manganese field, such as the sturmanite group of minerals and the calcium-hydroxy-silicate minerals, including xonotlite, tobermorite, and the carbonates rhodochrosite, kutnohorite, and calcite, precipitated from highly saline hydrothermal fluids as hydrothermal fluid flow ceased and the remaining fluids cooled. Spectacular mineral associations, with large euhedral crystals could, of course, only form where undisturbed crystal growth was possible (i.e., in open space provided by veins and fractures and in dissolution cavities that range in size from microscopic pore spaces to openings several cubic meters in size).

Next month we start to take a look at the minerals of the Kalahari manganese field.

Mineral of the month 

Emerald

Emerald is the most valuable of gems. It is the transparent green variety of the beryllium alumino silicate mineral beryl that owes it's green color to small amounts of chromic oxide. It is a relatively hard stone, 7.5 on the Moh's scale. The emerald (Greek: Smaragdos) of the ancients probably referred to a number of green stones. Lacking the fire and brilliance of the diamond, emerald is usually step cut, with elongated narrow facets and an oblong table, to enhance its color.

Emerald has been obtained from the schists of Cleopatra's mines, rediscover in 1818 in the Sikiat-Zubara region of Egypt. Vast quantities were taken from South America during the Spanish conquest, but the original mines have since been lost. The finest stones come from Columbia where they are mined from the calcite veining bitumous limestone at Muzo, Cosauez, and Somodocco and Bogoti.

The Emeralds that we have in our facet stone section comes from Zimbabwe and they are known as the Sondawana emeralds. They have stunning color and is known for the inclusions inside. Some emerald have also been found in Zambia. A lot of superstition surrounds the emerald.

Zambian emerald although discovered in the late 40's was not commercially mined until the 1950's. Today Zambia is one of the worlds's leading producers of fine Emerald. Highly prized for its intense color and remarkable clarity, Zambian Emerald retains its magnificent hue even in small stones of less than 0.5 ct. Although the experienced professional could identify a Zambian emerald in a Bond Street window, the chances are that it will be sold as a 'Sandawana' stone since the exporting of Zambian rough has long been considered a clandestine event and therefor does not lend itself well the respectability projected by the top jewelers shops of the world.

Much legend, lore and illusion are used by the trade when it comes to selling a fine emerald. Antiquity now seems to be the order of the day. Some dealers refer to emeralds as "Old Mine" and offer wonderfully supportive tales as to how the stone found its way through the centuries. Although much research has been done to establish the source of the 'Old Mine' (believed to have been in India) it still remains a mystery. This does not appear to deter the buyer and 'Old Mine' stones have been known to change hands for as much as US$ 30,000 per carat. 

Colombia, much sought after for the large crystals and therefore bigger stones. However the material does not suit small stones and invariably is more included than its Zambian brother.

Zimbabwe: Sandwana mine is well known for its similarity to Zambian material. Steady production from this mine has been bolstered by Zambia’s illegal exports, rendering an even greater reputation as a reliable source.

Brazil, Madagascar, Mozambique, Russia and Nigeria also produces an 'Emerald' colored by vanadium but it is not intentionally recognized as emerald since the chromium content is too low.

It is the birthstone of May. It is treated with colorless oil or wax, or natural and synthetic resins into voids to improve appearance. Surface cavities of emeralds is commonly filled with a hardened colorless substance.

Superstitions abound concerning the emerald, birthstone for May: it supposedly soothes the eyes, preserves chastity, cures dysentery, prevents epilepsy, drives away evil spirits, and facilitates childbirth symbolizes youth and rebirth and  believed by the ancients to empower the owner with foresight into the future.

As one of the most revered of all gemstones, Emeralds are a variety of the mineral Beryl and are mined in Columbia, Brazil, and Zambia. They are cut in a number of different shapes including round, marquise, oval, pear shapes, squares, cabochon, as well as the traditional emerald cut or step-cut shape.

Emeralds are graded principally according to color, clarity and shape. For simplicity, the grades are usually called Commercial, Good, Fine, and Extra Fine. Each grade represents a range of qualities.

Emerald Enhancements

Most emeralds have inclusions which can be regarded as its natural birthmarks that distinguish them as truly natural gemstones. Early gem merchants from India sought to enhance the color of emeralds by immersing them in clear oils and paraffin. They discovered that clear oils and waxes rendered surface fractures nearly invisible to the naked eye.

Today, most emeralds are oiled. Oiling is the oldest and most widely used treatment and is done in most places in the world. It is a process used to enhance the clarity of emeralds and is relatively easy to identify by a gemologists. In practice, clear oil is applied to the emerald and seeps into the emerald through surface fractures. Oiling is generally not permanent and may need to be reaplied every few years. While colorless oil is considered an acceptable practice, the use of green oil is considered a deceptive practice.

Today, there are many sophisticated techniques with which to improve the clarity of emeralds. In addition, to oils and waxes, there are now clear resins called Opticon that is sometimes applied to an emerald that seals surface fractures. In contrast to oiling, Opticon is loner lasting. Opticon is considered an acceptable practice, except when green dye is used to enhance the emerald's color.

Emerald Value

Emeralds are one of the most rare and valuable of all gemstones. While commercial grade emeralds are quite plentiful, fine and extra fine quality emeralds are very, very, rare. For purposes of illustration the following table indicates the range of retail prices that could be typical for a 1 carat emerald ( prices are for comparison only, exact prices vary according to market demand).

  • Quality Grade Low to High Retail Price Range for 1.0 Carat Emerald 

  • Commercial $30.00 to $525.00 

  • Good $525.00 to $1,125.00 

  • Fine $1,125.00 to $2,900.00 

  • Extra Fine $2,900.00 to 9,800.00 

Similar to other gemstones, larger emeralds are much more rare than smaller sizes. Accordingly, larger emeralds command much higher prices. For instance, while a one carat (1.0 ct.) good quality emerald may sell for somewhere between $525 and $1,125, a five carat (5.0 ct.) emerald of similar quality could sell for between $7,500 and $15,000 ( prices are for comparison only, exact prices vary according to market demand).

  • Quality Grade Low to High Retail Price Range for 5.0 Carat Emerald 

  • Commercial $300 to $7,500 

  • Good $7,500 to $15,000 

  • Fine $15,000 to $32,500 

  • Extra Fine $32,500 to $95,500 

The effect of oiling or the use of Opticon on the price of an emerald depends on its quality. For most qualities of emerald sold in jewelry, the effect on the price is negligible. However, for fine to extra fine emeralds, a non-oiled gemstone could command from 30% to 60% higher

    The rich green emerald holds within it the promise of new life in springtime. How appropriate that it should also be considered the May birthstone.

Long ago the emerald was dedicated to Venus, the goddess of love. Lovers were told that this gemstone could reveal the faithfulness of their beloved. Faithfulness was reflected in a fresh, bright green color; a cheating heart was betrayed by a lifeless color.

    Emeralds have always been highly prized by royalty. Cleopatra, queen of Egypt wore emeralds from her mine in Upper Egypt. Emeralds are heavily represented in the Russian Crown Jewels from the time of the czars. The Emperor Nero is said to have gazed through a large emerald to soothe his eyes as he watched the gladiator games in the Coliseum.

The ancients prized the emerald highly and believed it held many powers. They felt it could endow the wearer with the ability to think clearly in the past, present and future. It was supposed to improve one's memory, promote eloquent speech, quicken intelligence and endow the ability to foretell the future. It was also believed to promote honesty and frugality. Powdered and taken as a medicine, it was considered a preventative of epilepsy and other serious disorders.

    Like many other gems, emerald had to share its earliest fame with other green gems which had not yet been recognized for their uniqueness. Also called emerald by the ancient Romans were green sapphire, turquoise, smithsonite, malachite, jasper and glass. According to the historian Pliny, the Romans believed that emeralds ripened into their color, so gems with light patches or consistent paleness were considered immature.

The emerald's exciting color has always been its lure. Even uncut, unpolished crystals are immediately recognized as something special. Indeed, when evaluating emeralds, color is the most important quality factor. Included crystals and cavities are not a hindrance unless they weaken the stone or cause it to appear cloudy or muddy. In fact, emerald inclusions often create a graceful, branch-like pattern known as a "jardin" (French for "garden").

A colorful history 

Colombia, South America has always been the source of the finest emeralds. When the Spaniards conquered the Incas in the early 16th century, they stole all the emeralds they could find. However, the Incas refused to reveal the source of these coveted gems, and fortunately, the jungle quickly grew over the paths to the mines. The precious treasure was safe from the plunderers---at least temporarily. In 1555 one of the mines of Muzo was discovered by accident, and the Spanish began mining.

    Colombian emeralds are a relatively clear pure green, slightly yellowish-green or slightly bluish-green. The only neighboring country to Columbia that is important as an emerald source is Brazil. Other sources are the African countries of Tanzania, Zambia and Zimbabwe.

The two most famous emeralds are the Devonshire and the Patricia. The Devonshire is a 1383.95-carat, uncut Colombian crystal of fine green color. It was given to the sixth Duke of Devonshire by Emperor Dom Pedro I of Brazil in 1831. It is on permanent loan to the British Museum of Natural History. The 630-carat Patricia Emerald is another crystal of fine color that resides in the American Museum of Natural History in New York City.

Duplicating nature 

Synthetic emeralds first became commercially available in the 1940's. This was a tremendous technological improvement over the imitations which had been substituting for emeralds for generations. The synthetic is physically, optically and chemically identical to the natural gemstone. It is the result of the scientist's attempt to duplicate nature's processes in the laboratory.

Jewelry fashioning 

The most popular cut for emeralds is a rectangular step cut. As a matter of fact, this cut is so widely used, the cut itself is often called the emerald cut. It is preferred because it shows fine color to the best advantage.

    Emeralds are used in a wide range of jewelry styles from dainty pinkie rings to the most extravagant emerald and diamond necklaces. Quality and prices vary just as much. Emeralds are popular as center stones in rings, earrings and pendants, either encircled or offset by diamonds. Small emeralds are often combined with diamonds in cluster rings or pins or set into an anniversary ring. They are sometimes carved into exciting ring stones or pendants

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