| Jet | |
|---|---|
&sq=Qlik&lang=&file=File:Sample_of_jet_2013.JPG) Sample of unworked jet, about 15 mm long | |
| 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.
- ^ Neuendorf, K. K. E. Jr.; Mehl, J. P.; Jackson, J. A., eds. (2005). Glossary of Geology (5th ed.). Alexandria, Virginia: American Geological Institute. p. 344.
- ^ Holmes, Ralph J.; Crowningshield, Robert (1983). "Gemology". In Fyfe, Keith (ed.). The Encyclopedia of Mineralogy. Encyclopedia of Earth Sciences Series. Springer. pp. 168–187. doi:10.1007/0-387-30720-6_51. ISBN 978-0-87933-184-9.
- ^ Oxford English Dictionary (2nd edition) 1989, Oxford, Oxford University Press
- ^ Pye, K. (1985). "Electron microscope analysis of zoned dolomite rhombs in the Jet Rock Formation (Lower Toarcian) of the Whitby area, U.K.", Geological Magazine, volume 122, issue 3, pp. 279–286, Cambridge University Press, doi:10.1017/S0016756800031496