|Variable, but rich in carbon|
|Color||Black, occasionally brown|
|Mohs scale hardness||2.5–4.0|
|Common impurities||Iron, sulfur|
Jet is a type of lignite, the lowest rank of coal, and is a gemstone. Unlike many gemstones, jet is not a mineral, but is rather a mineraloid. 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. Jet is either black or dark brown, but may contain pyrite inclusions 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. Jet is found in two forms, hard and soft. Hard jet is the result of carbon compression and salt water; soft jet may be the result of carbon compression and fresh water. 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.
Jet is around 75% carbon and 12% oxygen with sulfur and hydrogen making up most of the balance. 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. 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.
Jet is very easy to carve, but it is difficult to create fine details without breaking so it takes an experienced lapidary to execute more elaborate carvings.
The jet found at Whitby, in England, is the "Jet Rock" 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. Whitby Jet is the fossilized wood from species similar to the extant Chilean pine (Araucaria araucana). The deposit extends throughout North York Moors National Park.
Jet was mined from a number of areas of France including Montjardin and Roquevaire. Raw jet was also imported from Spain. 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. An 1871 plan to import raw French jet into Whitby was unsuccessful due to its poor quality.
The jet found in Asturias, the biggest deposit in northern Spain, 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.
Native American Navajo and Pueblo tribes of New Mexico were using regionally mined jet for jewellery and the ornamentation of weapons when early Spanish explorers reached the area in the 1500s. 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 and the Front Range of El Paso County, Colorado.
Jet has been used in Britain since the Neolithic period It continued in use in Britain through the Bronze Age where it was used for necklace beads. Jet necklaces following the plate and spacer design may have been based on Gold lunula. 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.
Early archaeologists (particularly Victorian) often failed to distinguish between jet and other jet-like materials  In particular in southern Britain the material described as jet was often Kimmeridge Shale. and some artifacts use more than one jet-like material. For example the Pen y Bonc necklace combines two or three jet pieces with other dark material.
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, rather it was transferred to Eboracum (modern York) where considerable evidence for jet production has been found. The collection of jet at this time was based on beachcombing rather than quarrying. It was used in rings, hair pins, beads, bracelets, bangles, necklaces, and pendants, many of which are visible in the Yorkshire Museum. Jet rings tended to follow the styles of existing metal rings although there were exceptions. Jet pendants were carved cameo style with Medusa head being a popular theme.
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. One item that has been found around the Rhine but not in Britain are jet bracelets that feature grooves with gold inserts.
In the Roman period it saw 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. 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." It has been referenced by other ancient writers including Solinus and Galen.
Vikings made some use of jet including rings and miniature sculptures of animals with snakes being a prominent theme. The source of the jet hasn't been confirmed although Whitby is the most likely possibility.
Jet as a gemstone became fashionable during the reign of Queen Victoria. 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. Later the Queen wore Whitby jet as part of her mourning dress while mourning the death of Prince Albert.
Jet use was at its highest in the early 1870s and from there it declined. From above 1000 workers in the trade Whitby was down to 300 by 1884. 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. At 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. Making tourist trinkets kept a few jewellers in work but by the end of World war 2 only 3 remained and the industry died out completely with their deaths.
In Whitby the Victorian tradition continued up until the aftermath of World war 2. Jet Jewellery (both vintage and new) was then to remain out of fashion until the late 70s. In the 80s there was a fashion for Jet beads and antique jet jewellery started to rise in value. New jewellers took up the production of Jet Jewellery.
Glass was used as a jet substitute during the peak of jet's popularity. When it was used in this way it was known as French jet or Vauxhall glass. Ebonite was also used as a jet substitute and initially looks very similar to jet, but it fades over time. In some cases jet offcuts were mixed with glue and molded into jewelry.
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.
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
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.
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