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JADEITE - Canadian Institute of Gemmology

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Black Jadeite. There are in fact two types <strong>of</strong> so-called black jadeite. One <strong>of</strong> these comes from<br />

Burma, and is really gray rather than black, and the other comes from Guatemala, and is truly black.<br />

Ou Yang and Hansheng (1999: 417-418) comment in regard to Burmese black jade that<br />

"currently the term 'black jade' may include different types <strong>of</strong> pyroxene jades and is potentially<br />

confusing for the trade." Since first appearing on the market in Burma in the mid-1990s, this type<br />

<strong>of</strong> jadeite has been used to make various forms <strong>of</strong> jewelry in Hong Kong and Taiwan, but it has not<br />

proven to be very popular. The color <strong>of</strong> this type <strong>of</strong> jadeite tends to be grayish-black rather than<br />

pure black. Since the color is said to be similar to that <strong>of</strong> black-skinned chickens, in Hong Kong it<br />

is sometimes referred to as "black-skin-chicken jadeite". It is usually found in the vicinity <strong>of</strong> rivers<br />

in the form <strong>of</strong> boulders and is relatively rare.<br />

Ou Yang and Hansheng (1999: 418-419) describe "black jade" from Burma as being "opaque<br />

(fine grained) to translucent (coarser grained) with a vitreous lustre except in a few areas where it<br />

tends towards an oily lustre; fresh and well-polished surfaces have a vitreous lustre." Unlike black<br />

nephrite, on polished surfaces black jadeite can exhibit star-like flashes in reflected light. Ou Yang<br />

and Hansheng (1999: 419) report that its hardness on the Moh's scale is about 7, its specific gravity<br />

ranges from 3.325 to 3.333, and its RI is 1.653-1.665. It is inert under both long-wave and short-<br />

wave ultraviolet light. In terms <strong>of</strong> its composition, the authors report (page 419) that it is "essentially<br />

monomineralic, consisting <strong>of</strong> 95% jadeite and about 5% accessory minerals and black pigments."<br />

The jadeite belongs to the jadeite-omphacite-diopside pyroxene series. The color is derived from the<br />

presence <strong>of</strong> black or dark opaque dust-like materials that are associated with minute inclusions that<br />

are distributed throughout the stone. The inclusions are comprised <strong>of</strong> metallic oxides and sulphides,<br />

amorphous carbon, organic salts, water, CO 2, and various hydrocarbons.<br />

In the case <strong>of</strong> Guatamalan "black jade", it was used in Prehispanic times to make celts and<br />

other artifacts. It is presently being used by lapidaries in Guatemala City and Antigua, Guatemala, to<br />

make various types <strong>of</strong> jewelry. Harlow and Donnelly (1989) describe its petrological features in<br />

Guatemala and Garza-Valdés (1993: 113) describes its chemical composition and related<br />

properties:<br />

Aegirine-augite (chloromelanite)-rich rocks, or black jade, are metamorphic rocks with a<br />

fine-grained-to-cryptocrystalline texture. The color is given by the pyroxene aegirine-augite<br />

(chloromelanite) and by taramite, a sodic-calciic amphibole (NaCaNaMgFe 2 2+.<br />

[AlFe 3+ ] 2Si 6Al 2O 22[OH] 2)... The amphibole is markedly pleochroic in blue, brown, and<br />

violet. This rock also contains titanite, albite, analcite, grossular, and white mica.<br />

Harlow (1993: 23) says that black jade in Mesoamerica "resembles basalt" and comments that "it is<br />

very durable... it takes a very good polish and shows little grain definition." Anna Miller (2001: 29)<br />

quotes Fred Ward about this black jadeite: "Black jadeite from the Moragua Valley area...<br />

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