Jet | |
---|---|
General | |
Category | Mineraloid |
Formula (repeating unit) | Variable, but rich in carbon |
Identification | |
Color | Black, occasionally brown |
Cleavage | None |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 2.5–4.0 |
Streak | Brown |
Specific gravity | 1.3–1.4 |
Optical properties | Isotropic |
Refractive index | 1.640–1.680 |
Dispersion | None; opaque |
Ultraviolet fluorescence | None |
Common impurities | Iron, sulfur |
References | [ citation needed ] |
Jet is a type of lignite, [1] the lowest rank of coal, and is a gemstone. Unlike many gemstones, jet is not a mineral, but is rather a mineraloid. [2] It is derived from wood that has changed under extreme pressure.
The English noun jet derives from the French word for the same material, jaiet (modern French jais ), ultimately referring to the ancient town of Gagae. [3] Jet is either black or dark brown, but may contain pyrite inclusions [4] which are of brassy colour and metallic lustre. The adjective "jet-black", meaning as dark a black as possible, derives from this material.
Jet is a product of decomposition of wood from millions of years ago, commonly the wood of trees of the family Araucariaceae. [5] Jet is found in two forms, hard and soft. [5] Hard jet is the result of carbon compression and salt water; soft jet may be the result of carbon compression and fresh water. [5] Despite the name they both occupy the same area of the Mohs scale with the difference being that soft jet is more likely to crack when exposed to changes in temperature. [6]
Jet is around 75% carbon and 12% oxygen with sulfur and hydrogen making up most of the balance. [7] Other elements are found at trace level and the exact ratios varying with the source; for example, Spanish jet contains more sulfur than Whitby jet. [7] Jet has a Mohs hardness ranging between 2.5 and 4 and a specific gravity of 1.30 to 1.34. The refractive index of jet is approximately 1.66. The touch of a red-hot needle should cause jet to emit an odour similar to coal. [8]
Jet may induce an electric charge like that of amber when rubbed. [7]
Jet is very easily cut using carving tools, but small pieces tend to break off, making it difficult to create fine details. It therefore takes an experienced lapidarist to execute more elaborate carvings.
The jet found at Whitby, in England, is the "Jet Rock" [9] unit of the Mulgrave Shale Member, which is part of the Whitby Mudstone Formation. This jet deposit was formed approximately 181 million years ago, during the Toarcian age of the Early Jurassic epoch. [10] [11] [12] Whitby Jet is the fossilized wood from species similar to the extant Chilean pine ( Araucaria araucana ). [13] The deposit extends throughout North York Moors National Park. [14]
Jet has also been found in Kimmeridge shale seams in Dorset. [15]
Jet was mined from a number of areas of France including Montjardin and Roquevaire. [16] Raw jet was also imported from Spain. [16] In the 18th century there was a jet working industry based around Sainte-Colombe-sur-l'Hers and La Bastide-sur-l'Hers but this declined with the start of the 19th. [16] An 1871 plan to import raw French jet into Whitby was unsuccessful due to its poor quality. [16]
The jet found in Asturias, the biggest deposit in northern Spain, [17] is of Late Jurassic (Kimmeridgian) age, about 155 million years old. Asturian jet is a perhydrous coal that suffered an anomalous coalification process and presents great material stability over long periods of time. [18] At the end of the Middle Ages, the trade of religious objects and amulets made of jet reached great development in Santiago de Compostela, with sales to pilgrims traveling the Camino de Santiago. However, the deposits were in Asturias, where simple objects such as beads and rosary beads were also made. Santiago de Compostela was the main sales point and the location of the workshops that produced artistic objects. Jet has also been extracted in the area of Utrillas, Gargallo, and Montalbán in the province of Teruel, although it is of lower quality than that from Asturias. [19]
Native American Navajo and Pueblo tribes of New Mexico were using regionally mined jet for jewelry and the ornamentation of weapons when early Spanish explorers reached the area in the 1500s. [20] Today these jet deposits are known as Acoma jet, for the Acoma Pueblo. Enormous coal deposits characterize the San Juan Basin of New Mexico and this geology is closely related to jet deposits mined in the Henry Mountains of Utah [21] and the Front Range of El Paso County, Colorado. [22]
Jet is also commercialized in Poland [23] and near Erzurum in Turkey, where it is known as oltu stone and is used to make prayer beads. [24]
The earliest known worked jet object is a 10,000 BC model of a botfly larva, from Baden-Württemberg, Germany, found among the Venuses of Petersfels. [25]
Jet has been used in Britain since the Neolithic period [26] It continued in use in Britain through the Bronze Age where it was used for necklace beads. [26] Jet necklaces following the plate and spacer design may have been based on Gold lunula. [27] During the Iron Age jet went out of fashion until the early 3rd century AD in Roman Britain. The end of Roman Britain marked the end of jet's ancient popularity. [26]
Early archaeologists (particularly Victorian) often failed to distinguish between jet and other jet-like materials [28] In particular in southern Britain the material described as jet was often Kimmeridge Shale. [28] [29] and some artifacts use more than one jet-like material. [30] For example, the Pen y Bonc necklace combines two or three jet pieces with other dark material. [30]
Whitby jet was a popular material for jewellery in Roman Britain from the 3rd century onward. There is no evidence for Roman jet working in Whitby itself, [26] rather it was transferred to Eboracum (modern York) where considerable evidence for jet production has been found. [31] The collection of jet at this time was based on beachcombing rather than quarrying. [26] It was used in rings, hair pins, beads, bracelets, bangles, necklaces, and pendants, [26] many of which can be seen in the Yorkshire Museum. Jet rings tended to follow the styles of existing metal rings although there were exceptions. [32] Jet pendants were carved cameo style with Medusa head being a popular theme. [33]
Stylistic similarities with jet items found in the Rhineland, and lack of any evidence for local manufacture, suggest that Eboracum-produced items were exported to that area. [34] One item that has been found around the Rhine but not in Britain are jet bracelets that feature grooves with gold inserts. [35]
The Roman period saw its use as a magical material, frequently used in amulets and pendants because of its supposed protective qualities and ability to deflect the gaze of the evil eye. [36] Pliny the Elder suggests that "the kindling of jet drives off snakes and relieves suffocation of the uterus. Its fumes detect attempts to simulate a disabling illness or a state of virginity." [37] It has been referenced by other ancient writers including Solinus [38] and Galen.
Vikings made some use of jet including rings and miniature sculptures of animals with snakes being a prominent theme. [39] The source of the jet has not been confirmed although Whitby is the most likely possibility. [39]
Medieval jet use appears to have been largely limited to religious items such as crosses and Rosary beads. [40] During the period there was a belief that water drunk from jet bowls could help with labour. [41] A jet bowl held in the Museum of London may have been designed to allow for this. [42]
Jet became a valued costume accessory in the 16th century. Mary, Queen of Scots, owned jet buttons and clothes embroidered with jet beads. [43] Elizabeth I bought 1000 "black jet bugle drops" to embroider headdresses in 1587. [44] Anne of Denmark ordered a gown of "double burret" silk in June 1597 loaded with jet passementerie and 360 jet buttons. The gown was too heavy to wear and she ordered it to be remade with less jet. [45]
Jet as a gemstone became fashionable during the reign of Queen Victoria. [46] It originally became fashionable in the 1850s after the queen wore a necklace of it as part of mourning dress for Princess Victoria of Saxe-Coburg and Gotha. [46] Later the Queen wore Whitby jet as part of her mourning dress while mourning the death of Prince Albert. [13] [47] [48]
In some jewellery designs of the period jet was combined with cut steel. [49]
Jet use was at its highest in the early 1870s and from there it declined. [50] From above 1000 workers in the trade Whitby was down to 300 by 1884. [50] While jet substitutes may have had an impact this appears to have been in a large part due to changes in fashion with Art Nouveau making little use of black jewellery. [50] As the numbers fell the remaining manufactures tended to stick with existing styles rather than attempting to adapt to new fashions resulting in demand falling further. [50] Making tourist trinkets kept a few jewellers in work, but by the end of World War II only three remained, and the industry died out completely with their deaths. [50]
In Whitby the Victorian tradition continued up until the aftermath of World War II. [50] Jet jewellery (both vintage and new) was then to remain out of fashion until the late '70s. [51] In the '80s there was a fashion for jet beads and antique jet jewellery started to rise in value. [52] New jewellers took up the production of jet jewellery. [52]
Glass was used as a jet substitute during the peak of jet's popularity. [53] [54] When it was used in this way it was known as French jet or Vauxhall glass. [53] [54] Ebonite was also used as a jet substitute and initially looks very similar to jet, but it fades over time. [55] In some cases jet offcuts were mixed with glue and molded into jewelry. [55]
Anthracite (hard coal) is superficially similar to fine jet, and has been used to imitate it. This imitation is not always easy to distinguish from real jet.
Some museums have produced reproductions of jet artefacts in epoxy resin. [56]
Unlike black glass, which is cool to the touch, jet is not cool, due to its lower thermal conductivity. When rubbed against unglazed porcelain, true jet will leave a brown streak, although bog oak, vulcanite, and lignite will do the same. [57]
When non destructive testing is required, X-ray fluorescence spectroscopy, combined with visual inspection (including under high magnification) and X-ray imaging, is generally effective, although it can be difficult to differentiate jet from lignite. [30]
Real jet, when placed in a flame, burns like coal and gives off a coal-like smell and produces soot. No other black "gemstone" behaves like this.
Amethyst is a violet variety of quartz. The name comes from the Koine Greek αμέθυστοςamethystos from α-a-, "not" and μεθύσκωmethysko / μεθώmetho, "intoxicate", a reference to the belief that the stone protected its owner from drunkenness. Ancient Greeks wore amethyst and carved drinking vessels from it in the belief that it would prevent intoxication.
Beadwork is the art or craft of attaching beads to one another by stringing them onto a thread or thin wire with a sewing or beading needle or sewing them to cloth. Beads are produced in a diverse range of materials, shapes, and sizes, and vary by the kind of art produced. Most often, beadwork is a form of personal adornment, but it also commonly makes up other artworks.
A bead is a small, decorative object that is formed in a variety of shapes and sizes of a material such as stone, bone, shell, glass, plastic, wood, or pearl and with a small hole for threading or stringing. Beads range in size from under 1 millimeter (0.039 in) to over 1 centimeter (0.39 in) in diameter.
Jewellery consists of decorative items worn for personal adornment such as brooches, rings, necklaces, earrings, pendants, bracelets, and cufflinks. Jewellery may be attached to the body or the clothes. From a western perspective, the term is restricted to durable ornaments, excluding flowers for example. For many centuries metal such as gold often combined with gemstones, has been the normal material for jewellery, but other materials such as glass, shells and other plant materials may be used.
Lignite, often referred to as brown coal, is a soft, brown, combustible sedimentary rock formed from naturally compressed peat. It has a carbon content around 25–35% and is considered the lowest rank of coal due to its relatively low heat content. When removed from the ground, it contains a very high amount of moisture, which partially explains its low carbon content. Lignite is mined all around the world and is used almost exclusively as a fuel for steam-electric power generation.
Lapis lazuli, or lapis for short, is a deep-blue metamorphic rock used as a semi-precious stone that has been prized since antiquity for its intense color. Originating from the Persian word for the gem, lāžward, lapis lazuli is a rock composed primarily of the minerals lazurite, pyrite and calcite. As early as the 7th millennium BC, lapis lazuli was mined in the Sar-i Sang mines, in Shortugai, and in other mines in Badakhshan province in modern northeast Afghanistan. Lapis lazuli artifacts, dated to 7570 BC, have been found at Bhirrana, which is the oldest site of Indus Valley civilisation. Lapis was highly valued by the Indus Valley Civilisation. Lapis beads have been found at Neolithic burials in Mehrgarh, the Caucasus, and as far away as Mauritania. It was used in the funeral mask of Tutankhamun.
Turquoise is an opaque, blue-to-green mineral that is a hydrous phosphate of copper and aluminium, with the chemical formula CuAl6(PO4)4(OH)8·4H2O. It is rare and valuable in finer grades and has been prized as a gemstone for millennia due to its hue.
Bituminous coal, or black coal, is a type of coal containing a tar-like substance called bitumen or asphalt. Its coloration can be black or sometimes dark brown; often there are well-defined bands of bright and dull material within the seams. It is typically hard but friable. Its quality is ranked higher than lignite and sub-bituminous coal, but lesser than anthracite. It is the most abundant rank of coal, with deposits found around the world, often in rocks of Carboniferous age. Bituminous coal is formed from sub-bituminous coal that is buried deeply enough to be heated to 85 °C (185 °F) or higher.
A necklace is an article of jewellery that is worn around the neck. Necklaces may have been one of the earliest types of adornment worn by humans. They often serve ceremonial, religious, magical, or funerary purposes and are also used as symbols of wealth and status, given that they are commonly made of precious metals and stones.
Tiger's eye is a chatoyant gemstone that is usually a metamorphic rock with a golden to red-brown colour and a silky lustre. As members of the quartz group, tiger's eye and the related blue-coloured mineral hawk's eye gain their silky, lustrous appearance from the parallel intergrowth of quartz crystals and altered amphibole fibres that have mostly turned into limonite.
Onyx is the parallel-banded variety of chalcedony, a silicate mineral. Agate and onyx are both varieties of layered chalcedony that differ only in the form of the bands. Onyx has parallel bands, while agate has curved bands. The colors of its bands range from black to almost every color. Specimens of onyx commonly contain bands of black or white or both. Onyx, as a descriptive term, has also been applied to parallel-banded varieties of alabaster, marble, calcite, obsidian, and opal, and misleadingly to materials with contorted banding, such as "cave onyx" and "Mexican onyx".
Azurite or Azure spar is a soft, deep-blue copper mineral produced by weathering of copper ore deposits. During the early 19th century, it was also known as chessylite, after the type locality at Chessy-les-Mines near Lyon, France. The mineral, a basic carbonate with the chemical formula Cu3(CO3)2(OH)2, has been known since ancient times, and was mentioned in Pliny the Elder's Natural History under the Greek name kuanos (κυανός: "deep blue," root of English cyan) and the Latin name caeruleum. Copper (Cu2+) gives it its blue color.
A mangala sutra, or tali, is a necklace that the groom ties around the bride's neck in the Indian subcontinent, in a ceremony called the Mangalya Dharanam during a Hindu wedding. The necklace serves as a visual marker of status as a married Hindu woman.
The Bovey Formation is a deposit of sands, clays and lignite, probably over 1000 feet thick. It lies in a sedimentary basin termed the Bovey Basin which extends from Bovey Tracey to Newton Abbot in South Devon, England. The Bovey Basin lies along the line of the Sticklepath Fault and owes its existence to subsidence along this fault. A smaller basin with similar deposits lies further northeast along the fault at Petrockstowe.
Cannel coal or candle coal is a type of bituminous coal, also classified as terrestrial type oil shale. Due to its physical morphology and low mineral content cannel coal is considered to be coal but by its texture and composition of the organic matter it is considered to be oil shale. Although historically the term cannel coal has been used interchangeably with boghead coal, a more recent classification system restricts cannel coal to terrestrial origin, and boghead coal to lacustrine environments.
A ring is a round band, usually made of metal, worn as ornamental jewelry. The term "ring" by itself denotes jewellery worn on the finger; when worn as an ornament elsewhere, the body part is specified within the term, e.g., earrings, neck rings, arm rings, and toe rings. Rings fit snugly around or in the part of the body they ornament, so bands worn loosely, like a bracelet, are not rings. Rings may be made of almost any hard material: wood, bone, stone, metal, glass, jade, gemstone or plastic. They may be set with gemstones or with other types of stone or glass.
The Hoxne Hoard is the largest hoard of late Roman silver and gold discovered in Britain, and the largest collection of gold and silver coins of the fourth and fifth centuries found anywhere within the former Roman Empire. It was found by Eric Lawes, a metal detectorist in the village of Hoxne in Suffolk, England in 1992. The hoard consists of 14,865 Roman gold, silver, and bronze coins and approximately 200 items of silver tableware and gold jewellery. The objects are now in the British Museum in London, where the most important pieces and a selection of the rest are on permanent display. In 1993, the Treasure Valuation Committee valued the hoard at £1.75 million.
Clinker is a generic name given to waste from industrial processes, particularly those that involve smelting metals, welding, burning fossil fuels and use of a blacksmith's forge, which commonly causes a large buildup of clinker around the tuyere. Clinker often forms a loose, dark deposit consisting of waste materials such as coke, coal, slag, charcoal, and grit. Clinker often has a glassy look to it, usually because of the formation of molten silica compounds during processing. Clinker generally is much denser than coke, and, unlike coke, generally contains too little carbon to be of any value as fuel. It is also applied to the byproduct of combustion and heating by those who use anthracite or lignite coal-fired boilers.
The Street House Anglo-Saxon cemetery is an Anglo-Saxon burial ground, dating to the second half of the 7th century AD, that was discovered at Street House Farm near Loftus, in the unitary authority of Redcar and Cleveland, England. Monuments dating back as far as 3300 BC are located in the vicinity of the cemetery, which was discovered after aerial photography revealed the existence of an Iron Age rectangular enclosure. The excavations, carried out between 2005 and 2007, revealed over a hundred graves dating from the 7th century AD and the remains of several buildings. An array of jewellery and other artefacts was found, including the jewels once worn by a young high-status Anglo-Saxon woman who had been buried on a bed and covered by an earth mound.
Ancient Roman jewelry was characterized by an interest in colored gemstones and glass, in contrast with their Greek predecessors who focused primarily on the production of high-quality metalwork by practiced artisans. Extensive control of Mediterranean territories provided an abundance of natural resources to utilize in jewelry making. Participation in trade allowed access to both semi-precious and precious stones that traveled down the Persian Silk Road from the East.
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: CS1 maint: postscript (link) (See Upper Lias.)