Sunday, April 19, 2009

Diavik Diamond Mine

Diavik Diamond Mine
The Diavik Diamond Mine, near Bathurst Inlet, Nunavut
The Diavik Diamond Mine, near Bathurst Inlet, Nunavut
Coordinates: 64°29′46″N 110°16′24″W / 64.49611°N 110.27333°W / 64.49611; -110.27333
Country Canada
Territory Northwest Territories
Area [1]
- Total 7.0 km2 (2.7 sq mi)
Elevation [1] 416 m (1,365 ft)
Website http://www.diavik.ca/

The Diavik Diamond Mine is a diamond mine in the North Slave Region of the Northwest Territories, Canada, about 300 kilometres (186 miles) north of Yellowknife.[2] It has become an important part of the regional economy, employing 700, grossing C$100 million in sales, and producing 8 million carats (1600 kg) of diamonds annually. The area was surveyed in 1992 and construction began in 2001, with production commencing in January 2003. It is connected by an ice road and Diavik Airport with a 5,235-foot (1,596 m) gravel runway regularly accommodating Boeing 737 jet aircraft.

The mine is owned by a joint venture between the Harry Winston Diamond Corporation and Diavik Diamond Mines Inc., a subsidiary of Rio Tinto Group. The lifespan of the mine is expected to be 16 to 22 years.

The mine consists of three kimberlite pipes associated with the Lac de Gras kimberlite field and is located on an island 20 square kilometres (8 sq mi) in Lac de Gras and is informally called East Island. It is about 220 kilometres (137 mi) south of the Arctic Circle.

In 2006 the ice road from Yellowknife to the Diavik mine, and neighboring mines, froze late and thawed early.[1] The Diavik mine was unable to truck in all the supplies needed for the rest of 2006 before the road closed and arrangements had to be made to bring the remainder of the supplies in by air.

On July 5, 2007 a consortium of seven mining companies, including Rio Tinto, announced they are sponsoring environmental impact studies to construct a deep-water port in Bathurst Inlet.[3][4] Their plans include building a 211 km (131 mi) road connecting the port to their mines. The port would serve vessels of up to 25,000 tonnes.

Argyle diamond mine

Argyle diamond mine
Argyle diamond mine is located in Australia
Argyle diamond mine
Argyle diamond mine (Australia)
Location Lake Argyle
State Western Australia
Country Australia
Owner
Company Rio Tinto Group
Website http://www.argylediamonds.com.au/
Production
Products Diamonds
History
Opened 1985


The Argyle diamond mine (16°42′44″S 128°23′51″E / 16.71222°S 128.3975°E / -16.71222; 128.3975Coordinates: 16°42′44″S 128°23′51″E / 16.71222°S 128.3975°E / -16.71222; 128.3975) is a diamond mine located in the Kimberley region of Western Australia. The Argyle mine is the largest diamond producer in the world by volume, although due to the low proportion of gem-quality diamonds, is not the leader by value. It is the only known significant source of pink diamonds, producing 90 to 95% of the world's supply.

The Argyle diamond mine is also notable for being the first successful commercial diamond mine exploiting a volcanic pipe of lamproite, rather than the more usual kimberlite pipe. Much earlier commercial attempts to mine diamonds from a lamproite pipe in Arkansas in the southern United States were unsuccessful; the lamproite pipe there is now contained within the Crater of Diamonds State Park. The Argyle mine is owned by the Rio Tinto Group, a diversified mining company which also owns the Diavik Diamond Mine in Canada and the Murowa diamond mine in Zimbabwe.

Description

A false-color NASA image of the Argyle mine. Blue colours show the location of the mine and its depressed elevation as a result of the open pit mining technique.

The mine covers about 450,000 square metres (110 acres), stretching in a mostly linear shape about 1600 metres (5,200 ft) long and 150 to 600 metres (500 to 2,000 ft) wide. The mine is of open pit construction, and reaches about 600 metres (1,900 ft) deep at its deepest point. The open cut is nearing the end of its life and is due to close in 2009.

An underground block cave mine is currently under development.

Location

The Argyle diamond mine is located in the Kimberley region in the far northeast of the Australian state of Western Australia. It is located to the southwest of Lake Argyle in the Matsu Ranges, about 550 kilometres (340 miles) southwest of Darwin. Because the mine is located about 120 kilometres (75 miles) from the nearest settlement (Kununurra), a complete residential camp has been constructed on site. Most of the 520 workers commute from Perth, over 2,000 kilometres (1,200 mi) away, for alternating two week shifts at the mine. The mine has encouraged local employment and has a large number of indigenous local people working within the mine.

Geology

The mine is the first successful commercial diamond mine (except alluvial mining operations) not located on a kimberlite pipe. The pipe is named "AK-1", although it is commonly simply called the "Argyle pipe".

The volcanic pipe is a diatreme, composed of olivine lamproite, present as tuff and lava. Peripheral volcanic facies suggest the lamproite eruption formed a maar. At the margins of the volcanic pipe the lamproite is mixed with a volcanic breccia containing shattered wall rock fragments mixed and milled by the eruption. Minerals in the marginal facies include zeolite minerals, micas, kaolinite and clays, typical of post-eruption hydrothermal circulation.

Diamonds are found within the intact core of the volcanic pipe, as well as within some of the marginal breccia facies and maar facies. However, some diamonds are considered to have been resorbed during the post-eruption cooling of the pipe and converted to graphite.

The diatreme pipe formed by explosive eruption of the lamproite magma through a zone of weakness in the continental crust.

The diamonds found at the Argyle pipe have been dated to about 1.58 billion years of age, while the volcano which created the pipe is aged between 1.1 and 1.2 billion years old. This represents a relatively short period during which diamond formation could have taken place (around 400 million years), which may explain the small average size and unusual physical characteristics of Argyle diamonds. Diamonds found in the Argyle pipe are predominantly eclogitic, meaning that the carbon is of organic origin (see Natural history of diamonds).

In addition to the pipe itself, there are a number of semi-permanent streams that have eroded away portions of the pipe and created significant alluvial deposits of diamonds. These deposits are also actively mined.

Production

The Argyle diamond mine leads the world in volume production of diamond, averaging annual production of 35 million carats (7,000 kg), or about one third of global production of natural diamonds. Production peaked in 1994, when 42 million carats (8,400 kg) were produced. Of this quantity only 5% is considered gem-quality, with the rest being either near-gem quality or industrial grade; this is somewhat below world averages of about 20% of mined diamonds qualifying as gem-grade. Since the mine's opening in 1985, it has produced over 600 million carats (120,000 kg) of diamonds.

Most of Argyle's gem quality production is in brown diamonds. These diamonds are usually difficult to sell, although Rio Tinto has seen some success in a decade-long marketing campaign to promote brown diamonds as champagne and cognac toned. In contrast, the company has no problems selling pink and red diamonds, which are very rare and in high demand, therefore commanding premium prices. The pink diamonds are processed and sold as polished diamonds by a specialised team based in Perth to customers world wide. The highlight of the coloured diamond industry calendar is the annual Pink Diamond Tender. Access to its collector's edition catalogue and website access in itself is highly sought after.

The mine has ore processing and diamond sorting facilities on site. Once diamonds are removed from the ore and acid washed, they are sorted and shipped to Perth for further sorting and sale. A significant quantity of diamonds are cut in India, where low costs of labor allow small diamonds to be cut for a profit; this is especially relevant to the Argyle mine, which on average produces smaller rough diamonds than other mines do.

Diamond characteristics

The diamonds produced at the Argyle diamond mine are of an average low quality. Only 5% of mined diamonds are of gem quality, compared to a worldwide average of 20%; of the remaining 95%, they are about evenly split between classifications of "near gem quality" and industrial grade. 80% of Argyle diamonds are brown, followed by 16% yellow, 2% white, 2% grey, and less than 1% pink and green. Despite the low production volume of pink and red diamonds, the Argyle mine is the only reliable source in the world, producing 90 to 95% of all pink and red diamonds. Most Argyle diamonds are classified as type 1a (see material properties of diamond), and have low levels of nitrogen impurities, their colour resulting instead from structural defects of the crystal lattice. Argyle diamonds tend to fluoresce blue or dull green under ultraviolet light, and blue-white under X-ray radiation. The most common inclusion is unconverted graphite, followed by crystalline inclusions of orange garnet, pyroxene, and olivine.

Reserves

Initial proven reserves of the Argyle mine were 61 million tonnes of ore, with an average ore grade of 6.8 carats (1.36 g) per or tonne, about 400 million carats (80,000 kg). Further estimated reserves of 14 million tonnes of ore, at a grade of 6.1 carats (1.22 g) per tonne (85 million carats, 17,000 kg), also existed. As of 2001, reserves and resources in the open-pit mined area contain 220 million tonnes of 2.5 to 3.0 carat (500 to 600 mg) per tonne graded ore, sufficient to sustain current production rates until 2007. The ore grades at the Argyle mine are unusually high, with most commercial diamond mines averaging grades of 0.3 to 1.0 carats (60 to 200 mg) per metric ton. Alluvial deposits of diamonds are believed to have been exhausted.

In 1995, drilling samples taken from about 300 metres below the floor of the pit indicated the possible presence of about 100 million tons of ore, with an estimated grade of 3.7 carats (740 mg) per ton. In 1998, it was decided to instead move mining operations toward the west ridge of the mine, where 64 million tons of ore graded at 2.6 carats (520 mg) per ton are located.

An exploration decline was constructed at a cost of A$70 million to evaluate the economics of mining diamonds from the diamoniferous pipes below the floor of the open pit; these reserves would be mined underground (via block caving), rather than the open pit method currently used. In late-2005 Rio Tinto Ltd concluded that the operation was economically feasible. Pre-production construction of the underground mine commenced in early to mid 2006

Economics

The Argyle diamond mine is economically feasible because its large reserves and high grade ore offsets a low average diamond weight value. The estimated value of Argyle diamond production is only US$7 per carat (US$35/g); this compares to values of 70 USD per carat ($350/g) for diamonds produced at the Diavik mine and US$170 per carat (US$850/g) at the Ekati mine, both in Canada.[1] However, Argyle has two to four times the concentration of diamonds (ore grade) of these mines. This makes extraction economically feasible, as mine costs are mostly related to the amount of ore processed, not the amount of diamond extracted.

Underground expansion

In 2005 Rio Tinto was given the go ahead to a future expansion project, moving it from an open pit to an underground mine.[1] The project is predominantly an underground construction requiring high quality development and engineering excellence. The Block Cave is expected to operate until 2018 using the latest in mining technology, including Sandvik's auto mining technology.

The project is due to be completed by 2010.

Crater of Diamonds State Park

Crater of Diamonds State Park

IUCN Category III (Natural Monument)
Crater of Diamonds State Park is located in Arkansas
Crater of Diamonds State Park
Location Pike County, Arkansas, USA
Nearest city Murfreesboro, Arkansas
Coordinates 34°02′00″N 93°40′21″W / 34.0334423°N 93.6724040°W / 34.0334423; -93.6724040Coordinates: 34°02′00″N 93°40′21″W / 34.0334423°N 93.6724040°W / 34.0334423; -93.6724040
Area 911 acres (3.69 km2)
Established 1972
Governing body Arkansas State Park System

The Crater of Diamonds State Park is an Arkansas State Park located near Murfreesboro in Pike County, Arkansas, USA containing the only diamond bearing site in the world that is open to the public.

Description

The Crater of Diamonds State Park is an 911-acre (3.69 km2) Arkansas State Park situated over an eroded lamproite volcanic pipe. The park is open to the public and, for a small fee, rockhounds and visitors can dig for diamonds and other gemstones. Park visitors find more than 600 diamonds each year of all colors and grades.[1] Over 25,000 diamonds have been found in the crater since it became a state park. Visitors may keep any gemstone they find regardless of its value (and some, as listed below, have been quite valuable).

In addition to diamonds, visitors may find semi-precious gems such as amethyst, agate, and jasper or approximately 40 other minerals such as garnet, phlogopite, quartz, baryte, and calcite.

The crater itself is a 37.5-acre (152,000 m2) plowed field. It is periodically plowed to bring the diamonds and other gemstones to the surface. The remainder of the park consists of a visitor center, interpretive Diamond Discovery Center, campground, picnic area, and Diamond Springs aquatic playground. A 1.3 mile (2 km) walking trail along the Little Missouri River is available for hikers.

The park is open throughout the year.

History

In August 1906, John Huddleston found two strange crystals on the surface of his 243-acre (0.98 km2) farm near Murfreesboro, Arkansas, and soon became known as the first person outside South Africa to find diamonds at their original source. The following month, Huddleston and his wife, Sarah, sold an option on the 243 acres (0.98 km2) to a group of Little Rock investors headed by banker-attorney Samuel F. (Sam) Reyburn, who undertook a careful, deliberate test of the property.

After 1906, several attempts at commercial diamond mining failed. The only significant yields came from the original surface layer, where erosion over a long period of time had concentrated diamonds. In the early period, 1907-1932, yields from this "black gumbo" surface material often exceeded thirty carats per hundred loads (standard 1600-pound tramload of the early period). Highest yields from the undisturbed subsurface material (described as "kimberlite" or volcanic breccia, by the U. S. Geological Survey) were two carats per hundred loads in 1908 and about two carats per hundred short tons (2000 pounds)in 1943-1944.

Because equipment of the early period usually included bottom screens with mesh larger than 1/16th, thousands of smaller diamonds were allowed to pass through. The bulk of these ended up in drainage cuts of varying depths all over the field and in the big natural drains on the east and west edges of the diamond-bearing section of the volcanic deposit (approximately 35 acres (140,000 m2) of volcanic breccia on the east side of the 80-acre (320,000 m2) "pipe"). In recent decades, those small diamonds have been the bread-and-butter of recreational diamond-digging.

Soon after the original diamond was found, a "diamond rush" created a boomtown atmosphere around Murfreesboro. According to old tales, hotels in Murfreesboro turned away 10,000 people in the space of a year. Supposedly these aspiring diamond miners formed a tent city near the mine which was named "Kimberly" in honor of the famous Kimberley diamond district in South Africa. On the other hand, all available evidence indicates the Town of Kimberly originated as a land-development venture in 1909, initiated by Mallard M. Mauney and his oldest son Walter on their land immediately south of Murfreesboro. The project failed soon afterward as the speculative boom generated by the diamond discovery collapsed. Today the Kimberly area is almost all cow pasture, owned by Mauney's descendants.

From 1951 to 1972, the crater hosted several private tourist attractions. The first, The Diamond Preserve of the United States, lasted only about one year. In late 1951, Howard A. Millar stepped in and salvaged the infant tourist industry. In April 1952, Millar and wife, Modean, launched their "Crater of Diamonds" attraction. Howard Millar, an accomplished writer and promoter, stirred unprecedented national publicity and drew enough visitors to sustain the operation. In March 1956, a visitor found the "Star of Arkansas" on the cleared surface. The rare beauty weighed 15.33 carats (3.07 g). Later, Roscoe Johnston opened a rival tourist attraction, the "Arkansas Diamond Mine," on the main part of the diamond field.

The rivalry between the two tourist operations left both in a weakened position. In 1970 the entire volcanic formation was consolidated by a private partnership which then reassigned the property to General Earth Minerals of Dallas, Texas. GEM expected to turn the property over for a profit, but ended up heavily indebted to GF Industries of Dallas. Upon default, GFI took the property in July 1971.

GEM consolidated the tourist operation as well as the property. GFI continued the attraction until it sold the 80-acre (320,000 m2) volcanic formation and some 800 acres (3.2 km2) surrounding to the State of Arkansas in March 1972, for $750,000. The tourist operation continued as the centerpiece of Crater of Diamonds State Park.

Due in part to the park, and also because Arkansas was the first place outside South Africa where diamonds were found at their original volcanic source, this special gem has come to be associated with the Natural State. A large diamond symbol has dominated the state flag since the early years. The Arkansas State Quarter, released in 2003, bears a diamond on its face.

Geology

The Crater of Diamonds volcanic pipe is part of a 95 million-year-old eroded volcano. The deeply sourced lamproite magma, from the upper mantle, brought the diamonds to the surface. The diamonds had crystallized in the cratonic root of the continent long before, and were sampled by the magma as it rose to the surface.

The lamproite diamond source is unusual, as almost all diamonds are mined from kimberlite and from alluvial deposits of diamonds weathered from kimberlite. The most prominent lamproite diamond source is the Argyle diamond mine in Australia.

Premier Mine

The Premier Mine is an underground diamond mine owned by Petra Diamonds. It is situated in the town of Cullinan, 40 kilometres east of Pretoria, Gauteng Province, South Africa. Established in 1902, it was renamed the Cullinan Diamond Mine in November 2003 in celebration of its centenary. The mine rose to prominence in 1905, when the Cullinan Diamond — at the time the largest gem diamond ever — was discovered here. It is also the only diamond mine in the world where blue diamonds have been discovered.

Premier Mine, South Africa
Modern mine operations

The discovery of the mine occurred in 1890 by a Dutchman named Fabricius. He was actually prospecting for Henry Ward, who had an option to purchase the Wessels estate within a certain amount of time. However, Mr. Ward did not have any money to actually purchase the land and could have only done so if the land held diamonds, since it would be easy to find investors for it then. Ward became very fortunate when only a small part of the Wessels estate actually fell within the Cape Colony, and it was upon that portion of the land that the mine was discovered.

Scores of sanitary pits had been dug close to the mine, but never on the mine itself, and therefore the mine had never been discovered until Fabricius dug a random hole of 10 feet deep through limestone and the yellow ground was found.

Although Ward had all the rights as agreed with Wessels when buying the bond for the land, things were not that simple. Scores of pits a few feet in size were dug, and people refused to leave the land even though they did not have any rights. The fight became more complex because the mine was only a few hundred meters from the boundary between the Colony and the Free State. It was the Free State who had given Ward all rights to the mine since under their law, all minerals found belong to the owners of the land.

In the end Ward's claim was established beyond any doubt. Money problems kept pursuing him which let him first part with 50% of the land which after some transactions ended up in the hands of De Beers. He finally parted with the other 50% as well and sold it to De Beers but under the following conditions: Ward could take over the mine for a period of five years in which he was allowed 5,000,000 loads (equal to 4,000,000 tons of diamond bearing ground). This referred to the so-called yellow ground and the first 8 feet (2.4 m) of limestone were discounted for (since limestone would not hold any diamonds).

Cullinan Diamond Mine sold to Petra Diamonds

De Beers, the world's biggest diamond producer, said on Thursday 22nd of November 2007 it had sold its historic Cullinan mine to a consortium led by Petra Diamonds.

Notable Discoveries

The Cullinan Diamond is the largest rough gem-quality diamond ever found, at 3,106.75 carats (621.35 g).[1] It was found by Frederick Wells, surface manager of the Premier Diamond Mining Company in Cullinan, Gauteng, South Africa, on January 25, 1905. The stone was named after Sir Thomas Cullinan, the owner of the diamond mine.

In May 2008, a sparkling 101.27 carats (20.25 g) diamond (about the size of a pingpong ball) mined from the Premier Mine sold for more than $6.2 million at Christie's in Hong Kong. Cut from a 460 carats (92 g) rough, the shield-shaped gem boasts 92 brilliant facets. While internally flawless, the stone has a slight imperfection on the surface that is imperceptible to the human eye, the auction house said. The stone sold Wednesday to a private buyer for $6.21 million, it said. It is the largest colorless diamond to appear on the auction market in the last 18 years, Christie's said. Only three colorless diamonds of more than 100 carats (20 g) have appeared at auction. All were sold in Geneva. Naming rights were granted to the new owner.

Jwaneng diamond mine

Jwaneng diamond mine

Jwaneng Diamond Mine, Botswana
Location Kalahari Desert
Country Botswana
Owner
Company Debswana
Production
Products Diamonds (14.3 million carats in 2003)
History
Opened 1982


The Jwaneng diamond mine is the richest diamond mine in the world and is located in south-central Botswana about 170 kilometers (110 miles) west of the city of Gaborone, in the Naledi river valley of the Kalahari. Jwaneng, meaning "a place of small stones", is owned by Debswana, a partnership between the De Beers company and the government of Botswana. It is the second newest of four mines operated by the company, having begun operations in 1982.

Jwaneng is an open pit mine. The mine produces 9.3 million tons per year of ore and an additional 37 million tons per year of waste rock. The mine is located on three kimberlite pipes that converge near the surface, covering 520,000 square metres at ground level. In 2003, the mine produced 14.3 million carats (2860 kg) of diamond. The recoverable ore grade at the mine is about 1.25 carats per ton (250 mg/t). As of 2005, known reserves will allow production at current levels to continue for 27 years. The high rate of diamond extraction, combined with high quality diamonds fetching excellent per weight prices, make the Jwaneng diamond mine the richest diamond mine in the world by value of recovered diamonds.

Jwaneng employs over 2,100 people. The mine also owns and operates a local hospital and Jwaneng Airport. The mine maintains an ISO 14001 certificate for environmental compliance, being the first mine in Botswana to achieve this certification in 2000. Jwaneng is known for its excellent safety record, winning multiple national and international safety awards.[1]

High-security administration building at top

The Enhanced Thematic Mapper Plus (ETM+) instrument on NASA’s Landsat 7 satellite acquired this image of the Jwaneng Diamond Mine on May 17, 2001. The arid, flat landscape that fills most of this image appears in varying shades of brown, crisscrossed by pale beige roads. The Jwaneng Diamond Mine appears in the upper left quadrant of the picture, and a residential area appears near the bottom center.

At the center of the diamond mine, a series of concentric circles cut deeper and deeper into the ground. Surrounding the pit is a network of roads and structures related to the mining operation.

The settlement southeast of the mine contrasts with the arid landscape as much as the mine does. Here, tiny dots of green hint at trees and grassy parks. The pale beige rectangles around the perimeter of this image are probably crops or fallow fields.[2]

The Jwaneng mining lease includes the Jwana Game Park, which includes a field unit of Cheetah Conservation Botswana. The game park is also host to the globally threatened Lappet-faced Vulture.

Catoca diamond mine

Catoca diamond mine

Satellite image of the mine from June 21st, 2001. The light red point in the north-east of the mine is a bush fire.
Country Angola
Owner
Company Alrosa (32.8%)
Endiama (32.8%)
Odebrecht (16.4%)
Diamond Finance CY BV Group (16.8%)
Production
Products Diamonds (2.6 million carats in 2001)
History


The Catoca diamond mine is the fourth largest diamond mine in the world, and is located in Angola. The mine is owned by a consortium of international mining interests, including Endiama (the state mining company of Angola) (32.8% ownership), Alrosa of Russia (32.8%), Odebrecht of Brazil (16.4%), and the Diamond Finance CY BV Group (16.8%). The mine is located on a kimberlite pipe.

The mine had production of 1.8 million carats (360 kg) in 2000 and 2.6 million carats (520 kg) in 2001. Catoca management has been actively expanding capacity at the mine, such that the owners plan to extract as much as 5 million carats (1,000 kg) in 2005. The mine's production is 35 % gem quality, compared to a global average of 20 %; the diamonds produced at Catoca have an average value of $75 to $100 USD per carat (375 to 500 $/g). Estimated reserves are 60 million carats (12,000 kg).

Friday, April 17, 2009

Goldsmith

.
A goldsmith is a metalworker who specializes in working with gold and other precious metals. Since ancient times the techniques of a Goldsmith have evolved very little in order to produce items of jewelry of quality standards. In modern times actual Goldsmiths are rare. Historically goldsmiths have also made flatware, platters, goblets, decorative and serviceable utensils, and ceremonial or religious items, but the rising prices of precious metals have curtailed the making of such items to a large degree. Goldsmiths must be skilled in forming metal through filing, soldering, sawing, forging, casting, and polishing metal. Traditionally, these skills had been passed along through apprenticeships, however, more recently Jewelry Arts Schools specializing solely in teaching goldsmithing and a multitude of skills falling under the jewelry arts umbrella are available. Many universities and junior colleges also offer goldsmithing, silversmithing and metal arts fabrication as a part of their fine arts curriculum.

The nature of gold

Coupled with aesthetic attractiveness and rarity, gold's physical properties have given gold and items made from it, an unparalleled place in human history. Gold is so malleable and ductile that even primitive tools can work it to a high level of detail. It is fairly easily "pressure welded", which is to say that two small pieces can be pounded together to make one larger piece, similar to clay. Gold is a noble metal— it does not react with most elements. That means it is usually found in its native form, that it will last virtually forever without oxidization and tarnishing, and that it is easily melted, fused and cast without the problems of oxides and gas that are problematic with bronzes, for example. Throughout history, people have found its lustre and color to be aesthetically pleasing.

Since prehistoric times, mankind has been able to simply pick up gold off the ground, and anyone with two rocks would be able to form it into some pleasing or useful item. A major part of that history has been played by those who work in gold: goldsmiths.

History

Gold has been worked by humans in all cultures where the metal is available, either indigenously or imported, and the history of these activities is extensive. Superbly made objects from the ancient cultures of Europe, Africa, India, Asia, South America, Mesoamerica, and North America grace museums and collections around the world. Some pieces date back thousands of years and were made using many techniques that are still used by modern goldsmiths.

In medieval Europe goldsmiths were organized in guilds and were usually one of the most important and wealthy of the guilds in a city. The guild kept records of members and the marks they used on their products. These records are very useful to historians, were they to survive. Goldsmiths often acted as bankers, since they dealt in gold and had sufficient security for the safe storage of valuable items. In the Middle Ages, goldsmithing normally included silversmithing as well, but the brass workers and workers in other base metals were normally in a separate guild since the trades were not allowed to overlap. Usually jewelers were goldsmiths.

The printmaking technique of engraving developed among goldsmiths in Germany around 1430, who had long used the technique on their metal pieces. The notable engravers of the 1400s either were goldsmiths, as was Master E. S., or the sons of goldsmiths, such as Martin Schongauer and Albrecht Dürer

The modern goldsmith

It has been said that goldsmithing is the only art which uses some aspect of all other arts. Thus a fully realized goldsmith might have a wide array of skills and knowledge at their disposal. Gold, being the most malleable metal of all, offers unique opportunities for the worker. In today's world a wide variety of other metals, especially platinum alloys, may also be used extensively. 24 karat gold is generally called fine gold, and is the starting place for working with gold. Usually the gold is alloyed into any of various blends and colors, and the goldsmith may have some skill in that process. Then the gold may be cast into some item, usually with the lost wax casting process, or it may be used to fabricate the work directly in metal. In the latter case, the goldsmith will use a variety of tools and machinery, including the rolling mill, the drawplate, and perhaps swage blocks and other forming tools to make the metal into shapes needed to build the intended piece. Then parts are fabricated through a wide variety of processes and assembled by soldering. It is a testament to the history and evolution of the trade that those skills have reached an extremely high level of attainment and skill over time. A fine goldsmith can and will work to a tolerance approaching that of precision machinery, but largely using only his eyes and hand tools. Quite often the goldsmith's job involves the making of mountings for gemstones, in which case they are often referred to as jewelers.


'Jeweller' however is a term mostly reserved for a person who deals in jewellery (buys and sells) and not to be confused with a goldsmith, silversmith, gemologist, diamond cutter and diamond setters.

For further insight into the art of goldsmithing see bench jewelers.

Notable goldsmiths

See Category:Goldsmiths and Category:Silversmiths