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Classification
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Mineral
Classification: |
Elements |
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Strunz 8th
Ed. ID:
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1/O.0-10
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Nickel-Strunz 10th
Ed. ID:
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1.CC.05 |
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1 : ELEMENTS (Metals and intermetallic alloys; metalloids and
nonmetals; carbides, silicides, nitrides, phosphides) C : Metalloids and
Nonmetals C : Sulfur-selenium-iodine
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Related
to: |
Sulphur
Group. Sulphur
- Selenium Series
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Crystal
Data
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Crystallography:
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Orthorhombic
- Dipyramidal
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Crystal
Habit:
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Crystals
dipyramidal, thick tabular and disphenoidal, to 20 cm;
also massive, reniform, and forming stalactites; as
a powder.
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Twinning:
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On
[101], [011], [110], rare.
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Physical
Properties
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Cleavage: |
[001]
Imperfect, [110]
Imperfect, [111]
Imperfect; parting on [111]
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Fracture: |
Conchoidal
to Irregular/Uneven
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Tenacity:
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Brittle
to somewhat Sectile
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Hardness
(Mohs): |
1.5
- 2.5
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Density:
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2.07 (g/cm3)
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Luminescence:
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None |
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Radioactivity:
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Not
Radioactive
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Other: |
With a low melting point of 113 degrees C. sulphur burns readily in air, with a
low blue flame, and gives off choking fumes of sulphur-dioxide - "rotten" egg
odor.
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Optical
Properties
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Color: |
Sulfur-Yellow
to Honey-Yellow, Yellowish Brown, Greenish, Reddish
or Yellowish Gray; may be Black from included organic
matter.
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Transparency: |
Transparent
to Translucent |
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Luster: |
Resinous
to Greasy |
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Refractive
Index: |
1.958
- 2.245 Biaxial ( + )
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Birefringence: |
0.2873
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Dispersion: |
Relatively
Weak; r < v |
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Pleochroism: |
Weak
to Distinct |
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Occurances
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Geological
Setting: |
A
sublimation product at volcanic fumaroles; a product
of the activity of biological micro-organisms; as a
result of low oxidation potential and highly acidic
chemical reactions in mineral deposits; formed by the
decomposition of sulfides, especially pyrite, during
mine fires; found in sedimentary rocks. |
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Common
Associations: |
Anhydrite,
Aragonite, Calcite, Celestine, Gypsum, Halite |
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Common Impurities: |
Se,
Te |
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Type
Locality: |
None
(Prehistoric) |
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Year
Discovered: |
Prehistory
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View
mineral photos: |
Sulphur
Mineral Photos and Locations |
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More
Information
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Mindat.org Webmineral.com |
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Sulphur
is a common mineral but faceted gems are very rare.
Sulphur (S) is a native element, probably the only one
other than Diamond (C) that is available as a faceted
gem. Faceted gems are very rare because Sulphur is so
difficult to cut due to its very low Moh's hardness
of 1.5 - 2.5 and it high heat sensitivity. Sulphur is
very brittle when heated because of its poor heat conductivity.
It can actually crack if held titghtly in a person's
hand. Sulphur also has a bad reputation for its strong
odor. This odor occurs when water mixes with Sulphur
and hydrogen sulfide (H2S)
gas is produced. Even moisture in the air can produce
small amounts of H2S
gas. But it is a powerfull odor which smells like rotten
eggs. However, if Sulphur mineral specimens and gems
are kept dry they will not emit a strong odor.
Sulphur
is available from many sources worldwide although fine
crystal specimens are somewhat rare. Notable occurances
include Michigan and Ohio, USA; Bolivia; Chile; Poland;
and Sicily.
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