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| Kröhnkite
was named to honor B.
Kröhnke,
who provided the first analysis of the mineral.
| Discovered
in 1876;
IMA
status:
Valid (pre-IMA; Grandfathered) |
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Chemistry
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Chemical
Formula: |
Na2Cu(SO4)2
• 2H2O
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Hydrated
Sodium Copper Sulfate |
Molecular
Weight: |
337.68 gm
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Composition: |
Sodium |
13.62 % |
Na |
18.35 % |
Na2O |
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Copper |
18.82 % |
Cu |
21.19 % |
Cu2O |
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Hydrogen |
1.19 % |
H |
10.67 % |
H2O |
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Sulfur |
18.99 % |
S |
47.42 % |
SO3 |
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Oxygen |
47.38 % |
O |
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100.00 % |
|
97.63 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Sulfates
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Strunz 8th
Ed. ID:
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6/C.16-10
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Nickel-Strunz 10th
Ed. ID:
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7.CC.30
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7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
C : Sulfates (selenates, etc.) without additional anions, with H2O
C : With medium-sized and large cations
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Related
to: |
Roselite Group.
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Members
of Group: |
Roselite Group:
Brandtite, Kröhnkite, Roselite, Rruffite, Wendwilsonite.
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Varieties: |
None
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Synonyms: |
Kroehnkite,
Krömkite, Krönnkite, Salvadorite (of Herz)
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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 pseudo-octahedral, equant to short prismatic along
[001] or [100], to 7 cm; typically they exhibit {110},
{011}, {010}, {021}, {111}, with over two dozen more
forms recorded. In crusts and aggregates, granular,
massive.
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Twinning:
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Common
on {101}, may be heart-shaped.
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Physical
Properties
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Cleavage: |
Perfect
on {010}; poor on {101}
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Fracture: |
Conchoidal
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Tenacity:
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Brittle
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Moh's
Hardness: |
2.5
- 3.0
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Density:
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2.90 (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: |
Readily
soluble in water.
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Optical
Properties
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Color: |
Sky-Blue
to pale Blue or Greenish Blue, becoming Green and opaque
on exposure; pale Blue to Colorless in transmitted light.
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Transparency: |
Transparent
to Translucent |
Luster: |
Vitreous
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Refractive
Index: |
1.544
- 1.601
Biaxial ( - )
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Birefringence: |
0.057
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Dispersion: |
Weak |
Pleochroism: |
None
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Occurances
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Geological
Setting: |
An
uncommon secondary mineral formed in the oxidized zone
of copper deposits, typically in very arid climates.
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Common
Associations: |
Atacamite,
Blödite, Chalcanthite, Antlerite, Natrochalcite (Chuquicamata,
Chile).
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Common
Impurities: |
None
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Type
Locality: |
Chuquicamata Mine, Chuquicamata District, Calama, El Loa Province, Antofagasta Region, Chile
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Year
Discovered: |
1876
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View
mineral photos: |
Kröhnkite
Mineral Photos and Locations |
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More
Information
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Mindat.org
Webmineral.com
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Kröhnkite
is a rare hydrated copper sulfate mineral that is very
soft with a Mohs hardness of 2.5 - 3.0. Hydrated means
that it contains water in its chemical formula meaning it is prone to dehydration and must be kept
protected. It is also readily soluble in water. Kröhnkite
is an uncommon
secondary mineral formed in the oxidized zone of copper
deposits, typically in very arid climates.
It is found in colors of sky-blue to greenish blue becoming
green and opaque on exposure. Faceted gems are extremely
rare but very attractive due to its wonderful colors.
Distribution:
In Chile, abundantly and in large crystals from Chuquicamata,
at Quetena, west of Calama, and at Collahuasi, Antofagasta;
from El Cobre de Mejillones and in the Incahuasi district,
Atacama. In Wheal Hazard, St. Just, Cornwall, England.
From the Recsk copper deposit, Mátra Mountains, Hungary.
At Capo Calamita, Elba, Italy. From Broken Hill, New
South Wales, Australia.
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