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Classification
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Mineral
Classification: |
Silicates |
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Strunz 8th
Ed. ID:
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8/H.23-20 |
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8 : Silicates H : Phyllosilicates (layered), Tetragonal or
pseudotetragonal layered structures [Si4O10]4- and others 23 : Chlorite group
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Crystal
Data
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Crystallography:
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Monoclinic
- Prismatic |
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Crystal
Habit:
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Crystals
are thin
to thick pseudohexagonal crystals, with tapering pyramidal
faces, to 10 cm
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Twinning:
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Twin
plane [001]; twin axis [310], composition plane [001].
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Physical
Properties
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Cleavage: |
[001]
Perfect
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Fracture: |
Uneven
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Tenacity:
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Laminae
flexible, inelastic
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Moh's
Hardness: |
2.0
- 2.5
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Density:
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2.64 (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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Optical
Properties
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Color: |
Bright Purple
to Deep Crimson Red |
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Transparency: |
Transparent,
Translucent, Opaque |
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Luster: |
Vitreous |
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Refractive
Index: |
1.597 - 1.600 Biaxial
( - ) or ( + ) |
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Birefringence: |
0.0030 |
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Dispersion: |
r
< v
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Pleochroism: |
Strong;
violet/crimson red
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Occurances
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Geological
Setting: |
In
chromite deposits, associated with clinochlore and uvarovite. |
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Type
Locality: |
Kop Krum Mine, Kop Daglari, Erzurum District, Eastern Anatolia, Turkey |
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Year
Discovered: |
1851
(Clinlchlore) |
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View
mineral photos: |
Kämmererite
Mineral Photos and Locations |
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More
Information
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Mindat.org
(Kämmererite) Mindat.org
(Chromian Clinochlore) Mindat.org
(Clinochlore) Webmineral.com
(Clinochlore) |
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Kämmererite,
or Chromian Clinochlore, is the very rare red to
purple Chromium rich variety of Clinochlore. It is a
very beautiful mineral with intense color. Kämmererite
is micaceous so it is extraordinarily difficult
to facet because of its perfect basal cleavage. Faceted
gems are extremely rare and those that exist are usually
very small.
The most notable current source of Kämmererite
is the Kop Krum Mine, Erzurum District, Eastern Anatolia,
Turkey.
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