Blackjack Gemstone

1. Black Jack Stone
2. Blackjack Gemstones

The blackjack is a brawling weapon usually consisting of nothing more than a lead-weighted leather sack attached at the non-weighted end to a lanyard or looped leather strap. It is primarily used to incapacitate an opponent by inflicting crushing blows.

Alternate Names

• bludgeon
• sap

Mens Genuine Semi Precious Natural Gemstone Stainless Steel Bead Bracelet Blackjack Jewelry Co. Over the past decade, Men's jewelry has taken off. Unfortunately the market seems unorganized without true direction. New and unique Styles are hard to come by; and when actually found are sold at exceptionally high prices.

1. Sphalerite ((Zn, Fe)S) is a mineral that is the chief ore of zinc.It consists largely of zinc sulfide in crystalline form but almost always contains variable iron.When iron content is high it is an opaque black variety, marmatite.
2. Black rutilated quartz gemstones may also be cut into beads or carved into large ornamental spheres. Black rutilated quartz gemstones mainly come from India, and another essential source is in Brazil. Black rutilated quartz gemstones earn a 7 out of 10 on the Mohs scale of hardness, so they are suitable for any jewelry application.

Game Mechanics

The standard blackjack has a weight of 3 lbs.

Note: To edit this table go to Template:Weapon table blackjack

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References

Sphalerite ((Zn, Fe)S) is a mineral that is the chief ore of zinc. It consists largely of zinc sulfide in crystalline form but almost always contains variable iron. When iron content is high it is an opaque black variety, marmatite. It is usually found in association with galena, pyrite, and other sulfides along with calcite, dolomite, and fluorite. Miners have also been known to refer to sphalerite as zinc blende, black-jack and ruby jack.

Chemistry[edit]

Black Jack Stone

The mineral crystallizes in the cubiccrystal system. Like other minerals with a cubic crystal structure, sphalerite may show a tetrahedral crystal habit. In the crystal structure, zinc and sulfur atoms are tetrahedrally coordinated. The structure is closely related to the structure of diamond. The hexagonal analog is known as the wurtzite structure. The lattice constant for zinc sulfide in the zinc blende crystal structure is 0.541 nm.^[4]

All natural sphalerites contain concentrations of various impurity elements. These generally substitute for the zinc position in the lattice. The most common are Cd and Mn, but Gallium, Germanium and Indium may also be present in relatively high concentrations (hundreds to thousands of ppm).^[5] The abundances of these elements are controlled by the conditions under which the sphalerite formed, most importantly formation temperature and fluid composition.^[5]

Varieties[edit]

Its color is usually yellow, brown, or gray to gray-black, and it may be shiny or dull. Its luster is adamantine, resinous to submetallic for high iron varieties. It has a yellow or light brown streak, a Mohs hardness of 3.5–4, and a specific gravity of 3.9–4.1. Some specimens have a red iridescence within the gray-black crystals; these are called 'ruby sphalerite'. The pale yellow and red varieties have very little iron and are translucent. The darker, more opaque varieties contain more iron. Some specimens are also fluorescent in ultraviolet light.

The refractive index of sphalerite (as measured via sodium light, average wavelength 589.3 nm) is 2.37. Sphalerite crystallizes in the isometric crystal system and possesses perfect dodecahedral cleavage.

Gemmy, pale specimens from Franklin, New Jersey (see Franklin Furnace), are highly fluorescent orange and/or blue under longwave ultraviolet light and are known as cleiophane, an almost pure ZnS variety.

Occurrence[edit]

Sphalerite is the major ore of zinc and is found in thousands of locations worldwide.^[2]

Sources of high quality crystals include:^[3]

Economic importance[edit]

Sphalerite is the most important ore of zinc. Around 95% of all primary zinc is extracted from sphaleritic ores. However, due to its variable trace element content, sphalerite is also an important source of several other elements, such as cadmium,^[6], gallium^[7]germanium,^[8] and indium.^[9]

Gemstone use[edit]

Crystals of suitable size and transparency have been fashioned into gemstones, usually featuring the brilliant cut to best display sphalerite's high dispersion of 0.156 (B-G interval), over three times that of diamond. Freshly cut gems have an adamantine luster. Owing to their softness and fragility the gems are often left unset as collector's or museum pieces (although some have been set into pendants). Gem-quality material is usually a yellowish to honey brown, red to orange, or green.

Gallery[edit]

• Tan crystal of calcite attached to a cluster of black sphalerite crystals

• Sharp, tetrahedral sphalerite crystals with minor associated chalcopyrite from the Idarado Mine, Telluride, Ouray District, Colorado, USA

• Elmwood calcite specimen sitting atop sphalerite

• Gem quality twinned cherry-red sphalerite crystal (1.8 cm) from Hunan Province, China

• Sphalerite crystals from Áliva, Camaleño, Cantabria (Spain)

• Purple fluorite and sphalerite, from the Elmwood mine, Smith county, Tennessee, US

• Shalerite crystal in geodized brachiopod

Blackjack Gemstones

See also[edit]

References[edit]

1. ^Sphalerite. Webmineral. Retrieved on 2011-06-20.
2. ^ ^abSphalerite. Mindat.org. Retrieved on 2011-06-20.
3. ^ ^ab'Handbook of Mineralogy'(PDF).
4. ^International Centre for Diffraction Data reference 04-004-3804, ICCD reference 04-004-3804.
5. ^ ^abFrenzel, Max; Hirsch, Tamino; Gutzmer, Jens (July 2016). 'Gallium, germanium, indium, and other trace and minor elements in sphalerite as a function of deposit type — A meta-analysis'. Ore Geology Reviews. 76: 52–78. doi:10.1016/j.oregeorev.2015.12.017.
6. ^Cadmium - In: USGS Mineral Commodity Summaries. United States Geological Survey. 2017.
7. ^Frenzel, Max; Ketris, Marina P.; Seifert, Thomas; Gutzmer, Jens (March 2016). 'On the current and future availability of gallium'. Resources Policy. 47: 38–50. doi:10.1016/j.resourpol.2015.11.005.
8. ^Frenzel, Max; Ketris, Marina P.; Gutzmer, Jens (2014-04-01). 'On the geological availability of germanium'. Mineralium Deposita. 49 (4): 471–486. Bibcode:2014MinDe..49..471F. doi:10.1007/s00126-013-0506-z. ISSN0026-4598. S2CID129902592.
9. ^Frenzel, Max; Mikolajczak, Claire; Reuter, Markus A.; Gutzmer, Jens (June 2017). 'Quantifying the relative availability of high-tech by-product metals – The cases of gallium, germanium and indium'. Resources Policy. 52: 327–335. doi:10.1016/j.resourpol.2017.04.008.

• Dana's Manual of Mineralogy ISBN0-471-03288-3
• Webster, R., Read, P. G. (Ed.) (2000). Gems: Their sources, descriptions and identification (5th ed.), p. 386. Butterworth-Heinemann, Great Britain. ISBN0-7506-1674-1

External links[edit]