Postby dognose » Sun Jan 09, 2022 6:20 am
The Use of Jet in Jewelry
United States Bureau of Mines Reports Increase in Demand for Jet, Following World War, at Discovery of Mine in Utah
WASHINGTON, D. C., March 21.—Results of the tremendous mortality of the World War are reflected in an increased demand for the mineral jet, which is used to a considerable extent in mourning jewelry, according to the Bureau of Mines, which has completed a study of the subject. The bureau reports the occurrence of a deposit of jet in Wayne County, Utah, of sufficient size to meet any demand for the material likely to arise. Despite recent activity in the production of this material, the jet industry has declined to only a fraction of its former importance. One of the principal causes of the disuse of jet in recent years has been the substitution of the more durable black onyx. This stone, possessing a superior hardness, wears better than jet, and retains its polish for an indefinite period. This onyx is artificially colored black by allowing chalcedony, which is somewhat porous, to absorb a solution of an organic substance like sugar, which is then carbonized by immersion in sulphuric acid. This treatment produces a jet black color in the stone. Owing to the cheapness with which this black onyx can be produced, and also its superior hardness, it is doubtful whether the jet industry will revive or that it will be profitable to develop the deposits in the United States.
Jet is a substance of organic origin and has been defined as a dense black lignite. Jet is characterized by the lustrous, intense black surface it displays when polished. It is due to this property that the expression “jet black” is so commonly used to imply intense blackness.
Jet possesses fair dielectric strength and is a poor conductor of heat. When rubbed, it acquires a static charge and draws particles toward it; from this property it has probably acquired the name “black amber.” It ignites readily and burns with a brilliant smoky flame, which gives off a strong bituminous odor.
Jet has been used for ornamental purposes since prehistoric times, according to Pliny. The name itself is derived from a river or town in Lycia called Gagas, hence the term “gagates,” which has been gradually shortened to jet. Buttons, rings, amulets, and other ornaments have been found in barrows of the Bronze Age in England. The abundance of jet in Britain has been referred to by Roman writers in the third century, and many ornaments of jet have been found associated with Roman relics.
Whitby, in Yorkshire, has long been famous as the source of much of the world’s finest jet. A large industry in mining and manufacturing has been developed there, which was of considerable importance until the gradual exhaustion of the deposits, and the substitution of jet from foreign sources caused a steady decline in the industry. The industry at Whitby Abbey was first mentioned in 1350. Little more is known until 1808, when the first workshop was established. In 1873, 200 workshops employing about 1,500 persons were in operation. The production for that was valued at £90,000. Since that date there has been a gradual decline, until at present the Whitby industry is small, irregular, and comparatively unimportant.
It is believed that jet has been formed by the metamorphosis of wood. Examination of jet with the microscope discloses woody structure, and the general structure of coniferous wood. From the manner in which jet occurs in the Yorkshire deposits, it seems probable that these conifers did not grow on the spot, but drifted out to sea, where they became waterlogged and sank to the bottom. They then became gradually buried in the slowly depositing mud, where, in the presence of salt water, and under increasing pressures as deposition continued, the woody structure was compressed and metamorphosed until jet resulted. The muds were converted into shales, which were subsequently elevated to their present position.
Other foreign deposits of jet have been developed in the province of Asturias, Spain, which at present supply much of the small demands of the Whitby jet carvers. Jet has also been produced in the province of Aude, France, and Wurtemburg, Germany.
In the United States, jet has been found in a number of localities, but it has never been systematically mined or marketed. The small amount occasionally produced has been sold as mineralogical specimens, and very little has been used for ornamental purposes. Jet of excellent quality has been found in many places in Colorado, associated with coal-bearing rocks, particularly in El Paso County. The interesting and apparently large deposit reported in Wayne County, Utah, is in the form of flattened-out trees, whose entire structure, including roots and bark, has been metamorphosed to jet. From their occurrence in the stratum it is apparent that at one time they were covered with several thousand feet of overburden, which produced an enormous pressure sufficient to close the pores of the wood and greatly reduce its volume. The accompanying heat was sufficient to metamorphose the woody structure to jet. Sufficient of the original structure has been retained to permit the identification of three kinds of trees. The jet occurs promiscuously throughout a stratum which has, been exposed about 14,000 feet. Conditions for mining this material are said to be favorable in case any demand for jet arises which would make the exploitation of these deposits possible.
The value of the world’s yearly production of jet is estimated at $20,000. After being carved and polished, the cost to the ultimate consumer is several times this figure. Practically all the production is from Spain, England, France and Germany. The value of jet produced in this country in 1921 was $460. The average selling price of rough jet in the Whitby district in England is approximately five shillings ($1.25) per pound.
Details of the investigations of the Bureau of Mines are given in Serial 2452, “Jet,” by W. M. Myers, assistant mineral technologist.
Source: The Jewelers' Circular - 28th March 1923
Trev.