Dictionary:
jade·ite (jā'dīt') ![]() |
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The monoclinic sodium aluminum pyroxene, NaAlSi2O6. Free crystals are rare. Jadeite usually occurs as dense, felted masses of elongated blades or as fine-grained granular aggregates. It has a Mohs hardness of 6.5 and a density of 3.25–3.35. It has a vitreous or waxy luster, and is commonly green but may also be white, violet, or brown.
Jadeite is always found in metamorphic rocks. It is associated with serpentine at Tawmaw, Burma; Kotaki, Japan; and San Benito County, California. It occurs in metasedimentary rocks of the Franciscan group in California and in Celebes. It is found in Tibet; Yunan Province, China; and Guatemala.
Jadeite is the more cherished of the two jade minerals, because of the more intense colors it displays. It is best known in the lovely intense green color resembling that of emerald. See also Jade; Pyroxene.
| Rock & Mineral Guide: jadeite |
Environment
Little known in place, usually in waterworn boulders; freed by weathering from masses formed in serpentine by alteration of a soda-rich rock (nepheline and albite can be altered to jadeite).
Crystal descriptionFree (pocket) crystals are known only from California. Usually in distinctly granular masses of somewhat elongated blades, which give thin slices strength (but coarser and less tough than the finer-textured nephrite masses). Individual Mexican crystals, commonly associated with albite, are coarser (to ƈ in., 1-2 mm across), and less uniformly translucent than high-quality Myanmar material. Polished slabs sometimes show a silky luster from parallel cleavage cracks.
Physical propertiesEmerald to light green, white, violet, lilac, malachite green. (Boulder surfaces weather to yellow, orange, or red-brown, and skins of this hue are often left on Chinese artifacts). Luster glassy to silky; hardness 6Ɖ-7; specific gravity 3.3-3.5; fracture difficult, splintery; cleavage prismatic. Translucent to opaque.
CompositionSodium aluminum silicate (15.4% Na 2 O, 25.2% Al 2 O 3 , 59.4% SiO 2 ; some varieties, particularly that of Mexican artifacts, quite high in CaO and mixed with albite).
TestsFuses easily to a bubbly white glass, with a yellow sodium flame coloration.
Distinguishing characteristicsDiffers from far more common nephrite by its easy fusion and yellow flame coloration. Distinguished in worked objects by its gravity, which also separates it from idocrase and massive grossular. Hardness tests readily distinguish jade from soft-mineral (serpentine, agalmatolite, fluorite) carvings without any need for gravity tests, which can be complicated for large objects.
OccurrenceUntil recent years jadeite has been something of a mystery mineral, but we now know of primary sources in Guatemala as well as several California occurrences of white or grayish jadeite. Boulders in which a few small freestanding crystals have been seen occur in San Benito Co., California, with additional finds in Clear Creek, between New Idria and Hernandez. All Mexican jadeite is in artifacts, from unknown sources. Little of the Guatemalan rough resembles the fine bluish Olmec or richly green Mayan material; the sources for these are yet undiscovered (probably gathered as stream boulders, so now unrecognized). "Chinese" jadeite is mostly found as boulders in streambeds in Myanmar and traded to the Chinese carving centers. Low-quality rough has been found in place at one locality in Japan.
RemarksA valuable material for gem purposes (almost transparent emerald green stones are very valuable); the larger, less translucent and colorful masses are widely used for carvings in China. Color is often spotty, and sometimes present only as thin green seams in paler material with a spotty color pattern that can encourage a carver to excise detracting grains in favor of holes. Jadeite can be dyed and/or bleached, and buyers should observe caution, especially with violet jadeite.
| Wikipedia: Jadeite |
| Jadeite | |
|---|---|
Jadeite |
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| General | |
| Category | Pyroxene group |
| Chemical formula | NaAlSi2O6 or Na(Al,Fe3+)Si2O6 |
| Identification | |
| Color | Apple-green, emerald-green, bluish green, leek-green, greenish white, white, may show green spots, rarely blue or violet; colorless in thin section |
| Crystal habit | Commonly massive, or fibrous, granular - prismatic crystals rare |
| Crystal system | Monoclinic prismatic |
| Twinning | Single and lamellar twinning on [100] and [001] |
| Cleavage | Good on [110] |
| Fracture | Splintery |
| Mohs scale hardness | 6 - 7 |
| Luster | Subvitreous, pearly on cleavages |
| Diaphaneity | Translucent |
| Specific gravity | 3.24 to 3.43 |
| Polish luster | vitreous to greasy[1] |
| Optical properties | Biaxial (+) |
| Refractive index | nα = 1.654 - 1.673 nβ = 1.659 - 1.679 nγ = 1.667 - 1.693 |
| Birefringence | δ = 0.013 - 0.020 |
| Dispersion | r > v; moderate to strong. |
| Ultraviolet fluorescence | Dark colors are generally inert. Light green - inert to weak white in long wave, generally inert in short wave; light yellow - inert to weak green in long wave, generally inert in short wave; white - inert to weak in long wave, generally inert in short wave; light purple - inert to weak white or weak brownish red in long wave, generally inert in short wave; some dyed lavender colors - moderate to strong orange in long wave, weaker in short wave [1] |
| References | [2][3][4] |
Jadeite is a pyroxene mineral with composition NaAlSi2O6. It is monoclinic. It has a Mohs hardness of about 6.5 to 7.0 depending on the composition. The mineral is dense, with a specific gravity of about 3.4. Jadeite forms solid solutions with other pyroxene endmembers such as augite and diopside (CaMg-rich endmembers), aegirine (NaFe endmember), and kosmochlor (NaCr endmember). Pyroxenes rich in both the jadeite and augite endmembers are known as omphacite.
Jadeite is formed in metamorphic rocks under high pressure and relatively low temperature conditions. Albite (NaAlSi3O8) is a common mineral of the Earth's crust, and it has a specific gravity of about 2.6, much less than that of jadeite. With increasing pressure, albite breaks down to form the high-pressure assemblage of jadeite plus quartz. Minerals associated with jadeite include: glaucophane, lawsonite, muscovite, aragonite, serpentine, and quartz.
Rocks that consist almost entirely of jadeite are called jadeitite. In all well-documented occurrences, jadeitite appears to have formed from subduction zone fluids in association with serpentinite.[5] Jadeitite is resistant to weathering, and boulders of jadeitite released from the serpentine-rich environments in which they formed are found in a variety of environments.
Jadeite's color commonly ranges from white through pale apple green to deep jade green but can also be blue-green (like the famous and recently rediscovered "Olmec Blue" jade), pink, lavender, and a multitude of other rare colors. Chloromelanite is a very dark green to black variety.[6] Color is largely affected by the presence of trace elements such as chromium and iron. Its translucence can be anywhere from entirely solid through opaque to almost clear. Variations in color and translucence are often found even within a single specimen. Currently, the best known sources of gem quality jadeite are California, Myanmar, New Zealand and more recently Guatemala; other localities of jadeite include Kazakhstan, Russia, British Columbia, Alaska, and Turkestan.
Jadeite is one of the minerals recognized as the gemstone jade. The other is nephrite. Jadeite from the Motagua Valley, Guatemala, was used by the Olmec and Maya peoples, as well as the indigenous peoples of Costa Rica. Typically, the most highly valued colors of jadeite are the most intensely green, translucent varieties, though traditionally white has been considered the most valuable of the jades by the Chinese, known for their carefully crafted jade pieces. Other colors, like "Olmec blue" jade, which is characterized by its deep blue-green, translucent hue with white flecking, are also becoming more highly valued because of its unique beauty and historical use by the Mesoamerican Olmec and also in Costa Rica[7]; however, this variety was only recently rediscovered and is only being minimally exploited by native Guatemalans. It is thus difficult to obtain and as yet too rare and little known to have attained great value as a gemstone. When purchasing jade, quality is determined by the degree of translucence, cleanness of color, and purity of color. Occasionally, other minerals like serpentine or quartz are sold as jade but the difference can be determined by cleavage and hardness.
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
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