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Amesite
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Discovered in 1876; IMA status: Valid (pre-IMA; Grandfathered)
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Chemistry
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Chemical
Formula: |
Mg2Al(SiAl)O5(OH)4
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Magnesium
Aluminum Silicate Hydroxide |
Molecular
Weight: |
278.68 gm
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Composition: |
Magnesium |
17.44 % |
Mg |
28.92 % |
MgO |
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Aluminum |
19.36 % |
Al |
36.59 % |
Al2O3 |
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Silicon |
10.08 % |
Si |
21.56 % |
SiO2 |
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Hydrogen |
1.45 % |
H |
12.93 % |
H2O |
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Oxygen |
51.67 % |
O |
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100.00 % |
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100.00 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Silicates
(Germanates)
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Strunz 8th
Ed. ID:
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8/H.27-100
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Nickel-Strunz 10th
Ed. ID:
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9.ED.15
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9 : SILICATES (Germanates)
E : Phyllosilicates D : Phyllosilicates with kaolinite layers composed of tetrahedral and octahedral nets
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Related
to: |
Serpentine
Group (also known as Kaolinite-Serpentine Group).
Several polytypes are known: 2H1, 2H2, 6R and others.
In 1976 it was reported in volume 61 of the American
Mineralogist that Amesite had the first reported natural occurrence of the 6R
polytype for a trioctahedral 1:1 layer silicate.
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Members
of Group: |
Serpentine
Group: Amesite,
Antigorite, Baumite, Berthierine, Brindleyite, Caryopilite,
Chrysotile, Clinochrysotile, Cronstedtite, Dickite,
Fraipontite, Greenalite, Halloysite, Kaolinite, Kellyite,
Lizardite, Manandonite, Nacrite, Népouite, Odinite,
Orthochrysotile, Parachrysotile, Pecoraite, Vorhauserite
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Varieties: |
Chromian
Amesite, Ferroamesite
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Synonyms: |
Amenite,
Amensite, Amesine, Septeamesite
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Crystal
Data
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Crystallography:
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Triclinic - Pedial
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Crystal
Habit:
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As
tapering pseudohexagonal prisms elongated along [001],
to 2 mm; also tabular.
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Twinning:
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Common
as six-fold sector twins on {001} and polysynthetic
twins || {010} prism edges.
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Physical
Properties
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Cleavage: |
Perfect
on {001}
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Fracture: |
Irregular/Uneven
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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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2.77
- 2.78 (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: |
Colorless,
white or pale green; pink to lilac (chromian)
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Transparency: |
Transparent
to Translucent |
Luster: |
Resinous, Waxy, Greasy, Sub-Metallic;
Pearly to somewhat Metallic on cleavage surfaces. |
Refractive
Index: |
1.597
- 1.615
Biaxial ( + )
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Birefringence: |
0.015
- 0.018
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Dispersion: |
Weak; r < v |
Pleochroism: |
None
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Occurances
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Geological
Setting: |
A
product of low-grade metamorphism of Al, Mg-rich rocks.
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Common
Associations: |
Vesuvianite,
Chlorite (Pensacola Mountains, Antarctica); Magnetite,
Rutile, Diaspore (Chester, Massachusetts, USA); Grossular,
Calcite, Diopside, Clinozoisite (Black Lake, Canada).
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Common
Impurities: |
None
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Type
Locality: |
Chester Emery Mines, Chester, Hampden Co., Massachusetts, USA
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Year
Discovered: |
1876
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View
mineral photos: |
Amesite
Mineral Photos and Locations |
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More
Information
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Mindat.org
Webmineral.com
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Amesite
was discovered
in 1876 and
named by Charles Upham Shepard in honor of James Tyler Ames (1810 - 1883), who was
an American inventor and part owner of the Chester Emery Mines
in Massachusetts and had a rare and unusual collection of minerals.
Amesite is a relatively rare phyllosilicate mineral that is found in only a
few locations worldwide. Amesite is usually found in
colors of white or colorless or pale green.
However,
at the occurance at the Saranovkii Mine, Urals Region,
Russia Amesite crystals are found in beautiful
shades of pinks and lilacs to purples. The colors are due
to the presence of chromium (Cr) in the Amesite formula. And as
it turns out, these attractive crystals have grown
on solid black Chromite. These colorful crystals can
be called "Chromian
Amesite". Although Amesite
crystals are typically too small to be faceted, the
Russian Chromian Amesite can be formed into beautiful druzy-style
gems covered in short, sparkling purple crystals.
Sometime
after its discovery, Amesite was considered to be a
variety of Chlorite and re-named Corundophilite.
Amesite was re-established as a distinct species by E. V. Shannon in 1920, although he
continued to refer to Amesite as a Chlorite. Dr. J. W. Gruner demonstrated
in 1944 that Amesite is a Serpentine. Amesite is now a member of the Serpentine
Group of minerals that includes other gem-type minerals
such as
Antigorite and Lizardite.
Locations
for finding Amesite are
the Type Locality at the Emery mine, Chester, Hampden
County, Massachusetts, USA. From the Lake Asbestos mine,
Black Lake, Quebec, Canada. In Antarctica, in the Dufek
mafic massif, Pensacola Mountains. From the Postmasburg
manganese deposits, Cape Province, South Africa. From
Russia, at the Saranovskoye chromite deposits, Northern
Ural Mountains. At Hällefors, Sweden. On Mt. Sobotka,
Silesia, Poland.
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Amesite
gems for sale:
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have not photographed our Amesite gems yet. Please
check back soon.
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