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| Cleavelandite
is named after Parker Cleaveland, a professor of geology and mineralogy at Bowdoin College in Maine during the early 1800s.
| Discovered
in 1815 (Albite).
IMA
status: Not Valid (Cleavelandite is a variety of Albite) |
|
Chemistry
|
|
|
Chemical
Formula: |
Na[AlSi3O8]
|
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Sodium
Aluminum Silicate |
Molecular
Weight: |
263.02 gm
|
Composition: |
Soldium |
8.30 % |
Na |
11.19 % |
Na2O |
|
Calcium |
0.76 % |
Ca |
1.07 % |
CaO |
|
Aluminum |
10.77 % |
Al |
20.35 % |
Al2O3 |
|
Silicon |
31.50 % |
Si |
67.39 % |
SiO2 |
|
Oxygen |
48.66 % |
O |
|
|
|
|
100.00 % |
|
100.00 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Silicates
(Germanates)
|
Strunz 8th
Ed. ID:
|
8/J.07-20
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Nickel-Strunz 10th
Ed. ID:
|
9.FA.35
|
|
9 : SILICATES (Germanates) F : Tektosilicates without zeolitic H2O A : Tektosilicates without additional non-tetrahedral anions
|
Related
to: |
Variety
of Albite. Feldspar Group. Plagioclase Series. Na-rich end member of the Albite-Anorthite
Series. Low- and high-temperature structural modifications exist.
Low- and high-temperature structural modifications are
recognized.
|
Synonyms: |
Clevelandite
|
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|
Crystal
Data
|
|
|
Crystallography:
|
Triclinic - Pinacoidal
|
Crystal
Habit:
|
(Albite)
Crystals commonly tabular || {010}, may be curved,
to 3 cm; divergent aggregates, granular, cleavable massive.
|
Twinning:
|
(Albite)
Common around [010] or {010}, giving polysynthetic striae
on {001} or {010}; many other laws, contact, simple
and multiple.
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Physical
Properties
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|
|
Cleavage: |
Perfect
on {001}, very good on {010}, imperfect on {110}
|
Fracture: |
Irregular/Uneven
to Conchoidal
|
Tenacity:
|
Brittle
|
Moh's
Hardness: |
6.0
- 6.5
|
Density:
|
2.60
- 2.65 (g/cm3)
|
Luminescence:
|
Fluorescent, Short UV=cherry-red blue, Long UV=white. |
Radioactivity:
|
Not
Radioactive
|
Other: |
F
|
|
|
Optical
Properties
|
|
|
Color: |
White
to Gray, Bluish, Greenish, Reddish; may be chatoyant.
|
Transparency: |
Transparent
to Translucent
|
Luster: |
Vitreous,
Pearly on cleavages
|
Refractive
Index: |
1.528
- 1.542 Biaxial ( + ), Biaxial ( - ) for high
variety
|
Birefringence: |
0.0090
- 0.0100
|
Dispersion: |
Weak;
r < v
|
Pleochroism: |
None
|
|
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Occurances
|
|
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Geological
Setting: |
A
major constituent of granites and granite pegmatites,
alkalic diorites, basalts, and in hydrothermal and alpine
veins. A product of potassium metasomatism and in low-temperature
and low-pressure metamorphic facies and in some schists.
Detrital and authigenic in sedimentary rocks. |
Common
Associations: |
Quartz,
Orthoclase, Muscovite, Biotite, "Hornblende"
|
Common
Impurities: |
Ca,
K, Mg |
Type
Locality: |
(Albite)
Finnbo (Finbo), Falun, Dalarna, Sweden |
Year
Discovered: |
(Albite)
1815 |
View
mineral photos: |
Cleavelandite
Mineral Photos and Locations |
|
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More
Information
|
|
|
|
Mindat.org
(Cleavelandite) Mindat.org
(Albite) Webmineral.com
(Albite)
|
|
|
Cleavelandite
is a platy variety of Albite which is a member of the
Feldspar Group of minerals that includes Albite,
Amazonite,
Andesine, Anorthite, Bytownite, Hyalophane, Labradorite,
Moonstone,
Oligoclase, Orthoclase, Sanidine
and Sunstone. Cleavelandite
is not a gemmy variety but forms a very attractive inclusion
in Quartz. Round, white "snow ball" Cleavelandite
inclusions in faceted Quartz are very collectable. Although
Albite is widespread, Cleavelandite inclusions in Quartz
are relatively rare. The best source seems to be Minas
Gerais, Brazil.
|
Cleavelandite
gems for sale:
We
have not photographed our Cleavelandite gems. Please
check back soon.
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