Classification
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Mineral
Classification: |
Halides
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Strunz 8th
Ed. ID:
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3/A.04-10
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Nickel-Strunz 10th
Ed. ID:
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3.AA.25
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3 : HALIDES A : Simple halides, without H2O A : M:X = 1:1, 2:3, 3:5, etc.
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Related
to: |
n/a
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Varieties: |
None
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Synonyms: |
Chlorammonium,
Chloride of Ammonium, Muriate of Ammonia, Sal-Ammoniac,
Sal Ammoniac
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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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Crystals usually trapezohedral {112} modified by {113} at times; less
commonly with gyroidal forms alone, or in combination. Dodecahedral;
cubic (rare). Crystals often exhibit curved or stepped faces and may
present a tetragnal or rhombohedral appearance due to suppression of
faces and distortion. Skeletal or dendritic aggregates. Crusts or
stalactitic masses; fibrous, earthy or mealy.
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Twinning:
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On
{111}, may be cyclic
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Parting: |
Translation gliding with T{011}, t[001]
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Physical
Properties
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Cleavage: |
Imperfect
on {111}
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Fracture: |
Conchoidal
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Tenacity:
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Between
brittle and sectile; very plastic
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Moh's
Hardness: |
1.5
- 2.0
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Density:
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1.532 (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: |
Water
Soluble
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Optical
Properties
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Color: |
White,
pale Gray, may be pale Yellow to Brown if impure; Colorless
in transmitted light.
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Transparency: |
Transparent
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Luster: |
Vitreous
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Refractive
Index: |
1.693
Isotropic; may be weakly anisotropic
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Birefringence: |
0.00
(Isotropic) Weakly birefringent at times, especially after mechanical deformation.
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Dispersion: |
n/a
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Pleochroism: |
None
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Occurances
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Geological
Setting: |
A
sublimation product around volcanic fumaroles; in burning
coal seams and waste piles; in guano deposits. The ammonia
usually is derived from organic matter. |
Common
Associations: |
Sulfur
(fumaroles); Realgar, Orpiment, Sulfur, Mascagnite,
Tschermigite (burning coal). |
Common
Impurities: |
n/a
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Type
Locality: |
possibly
Etna, Vesuvius, Italy |
Year
Discovered: |
1546
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View
mineral photos: |
Sal
ammoniac
Mineral Photos and Locations |
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More
Information
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Mindat.org Webmineral.com
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Salammoniac is
a rare Halide mineral composed of ammonium chloride
(NH4Cl). Salammoniac is very difficult to facet because
it is water soluble, very soft (Mohs hardness of 1.5
-2.0) and has a very low specific gravity of 1.5. It
forms as some of the most interesting and collectable
crystal shapes in the mineral world. These complex,
intricate crystals are white to colorless and often
shaped like twisted spines with four sets of crystals
radiating out from and twisting around the center spine
at 90 degrees from each other.
Salammoniac is
a sublimation product that forms around volcanic
fume release vents or fumaroles. The crystallization
occurs as volcanic gases escape. Another natural occurrence
is from underground burning coal seams. The ammonia
usually is derived from organic matter. Notable occurrences include Tajikistan; Mt.
Vesuvius, Italy; and Parícutin, Michoacan, Mexico. The
localtion most known for the unique "spine-like"
crystals is the former Ravat Village,
Yagnob River, Viloyati Sogd, Tajikistan.
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