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| Chemistry:
Au
[Elemental
Gold] | Discovered
in Prehistory;
IMA
status: Valid (pre-IMA; Grandfathered). Gold
is an Old English word for the metal; perhaps related
to the Sanskrit jval; chemical symbol (Au) from
the Latin word aurum, meaning shining dawn. |
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Classification
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Mineral
Classification: |
Elements |
Strunz 8th
Ed. ID:
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1/A.01-10
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Nickel-Strunz 10th
Ed. ID:
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1.AA.05 |
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1 : ELEMENTS (Metals and intermetallic alloys; metalloids and
nonmetals; carbides, silicides, nitrides, phosphides) A : Metals and
Intermetallic Alloys A : Copper-cupalite family
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Related
to: |
Copper
Group. Gold - Silver Series. Gold - Palladium Series.
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Crystal
Data
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Crystallography:
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Isometric
- Hexoctahedral
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Crystal
Habit:
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As
octahedra, dodecahedra, and cubes, typically crude or
rounded, to about 5 cm. In twinned and parallel crystal
groups; reticulated, dendritic, arborescent, platy,
filiform, spongy; massive, and in rounded nuggets; scales
and flakes.
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Twinning:
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Common
on [111]; repeated to form reticulated and dendritic
aggregates.
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Physical
Properties
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Cleavage: |
None
Observed
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Fracture: |
Hackly,
Jagged
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Tenacity:
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Highly
Malleable and Ductile
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Hardness
(Mohs): |
2.5
- 3.0
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Density:
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19.30 (g/cm3)
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Luminescence:
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None |
Radioactivity:
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Not
Radioactive
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Other: |
Highly
Conductive
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Optical
Properties
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Color: |
Yellow, pale Yellow, Orange, Yellow White, Reddish White
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Transparency: |
Opaque |
Luster: |
Metallic |
Refractive
Index: |
R:
(400) 36.8, (420) 36.8, (440) 36.4, (460) 36.1, (480)
36.7, (500) 45.3, (520) 62.5, (540) 75.0, (560) 82.2,
(580) 86.8, (600) 89.7, (620) 91.9, (640) 93.3, (660)
94.1, (680) 94.8, (700) 95.3 |
Birefringence: |
0.00
(Opaque) |
Pleochroism: |
None |
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Occurances
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Geological
Setting: |
Widespread
in very small q\uantities in rocks of many kinds throughout
the world, and in sea water. In veins of epithermal
origin, typically in quartz with pyrite and other sulfides,
and with tellurides; in pegmatites; in contact metamorphic
deposits. Common in placers. |
Common
Associations: |
Altaite,
Ankerite, Arsenopyrite, Calaverite, Chalcopyrite, Krennerite,
Pyrite, Pyrrhotite, Quartz, Scheelite, Sylvanite, Tetradymite,
Tourmaline, |
Common
Impurities: |
Ag,
Cu, Pd |
Type
Locality: |
Prehistic |
Year
Discovered: |
Prehistic |
View
mineral photos: |
Gold
Mineral Photos and Locations |
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More
Information
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Mindat.org Webmineral.com |
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Gold
is a native element and precious
metal and has long been prized for its beauty, resistance to chemical attack
and workability. As it is found as a native
element, has a relatively low melting point (1063 degrees Celsius) and is
malleable, it has been used by mankind for thousands of years. Gold is
also used as a standard for international currency and is widely used in
jewelry, electronics (where its superb properties as a conductor help offset its
tremendous cost), dentistry and in photographic processes.
Gold occurs
in significant amounts in three main types of deposits: veins of hydrothermal
and related origin; in consolidated placer deposits, and in unconsolidated
placer deposits. It may also occur in granitic pegmatites, in contact
metamorphic deposits, and in hypo-thermal deposits. It is commonly found as
disseminated grains in Quartz veins with Pyrite and other sulphides, or as rounded grains, flakes or
nuggets in placer deposits and in streams and rivers. Gold is often panned from
such deposits by taking advantage of its high density to wash away the lighter
sediments from a pan or sluice.
There
are many localities worldwide for fine gold specimens
for mineral collectors and native Gold cabochons.
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Gold
gems for sale:
We
have not photographed our Gold gems. Please
check back soon.
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