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| Antigorite
was named in 1840 by Mathias Eduard Schweizer for the type locality, Valle
di Antigorio, Domodossola, Piedmont, Italy; although there is some question whether
it was found on the Italian side or the Swiss side
of the border.
| Discovered
in 1840;
IMA
status:
Valid (pre-IMA; Grandfathered) |
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Chemistry
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Chemical
Formula: |
(Mg;Fe2+)3Si2O5(OH)4
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Magnesium
Iron Silicate Hydroxide |
Molecular
Weight: |
300.77 gm
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Composition: |
Magnesium |
18.18 % |
Mg |
30.15 % |
MgO |
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Iron |
13.93 % |
Fe |
17.92 % |
FeO |
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Silicon |
18.68 % |
Si |
39.95 % |
SiO2 |
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Hydrogen |
1.34 % |
H |
11.98 % |
H2O |
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Oxygen |
47.88 % |
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.27-10
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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). Polymorphous with Clinochrysotile, Lizardite,
Orthochrysotile, and Parachrysotile.
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Members
of Group: |
Serpentine
Group (also known as Kaolinite-Serpentine
Group): Amesite, Antigorite, Berthierine, Brindleyite,
Caryopilite, Chrysotile, Clinochrysotile, Cronstedite,
Dickite, Fraipontite, Greenalite, Halloysite, Kaolinite,
Kellyite, Lizardite, Manandonite, Nacrite, Népouite,
Odinite, Orthochrysotile, Parachrysotile, Pecoraite
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Varieties: |
Al-Antigorite,
Andes Jade, Bowenite, Jenkinsite, Picrolite, Picrosmine,
Vorhauserite, Webskyite, Williamsite
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Synonyms: |
Baltimorite,
Bastard Asbestos, Genthite, Gymnite, Iron-Gymnite, Nickel-Gymnite,
Porcellophite, Protoantigorite, Septeantigorite, Thermophyllite,
Yu yen shi stone, Yu yen stone, Zermattite
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Crystal
Data
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Crystallography:
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Monoclinic
- Domatic
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Crystal
Habit:
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Minute
crystals, typically platy along [001], rarely elongated
along [010]; some plates have rectangular outline due
to cleavage; commonly bladed or fibrous.
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Twinning:
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May
exhibit two- or three-fold twins rotated 60° about an
axis [001].
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Physical
Properties
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Cleavage: |
Perfect
on {001}, observed on {100} and {010}
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Fracture: |
Conchoidal
or Splintery
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Tenacity:
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Brittle
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Moh's
Hardness: |
3.5
- 4.0
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Density:
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2.50
- 2.60 (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: |
Green,
Blue-Green, White; Colorless to pale Green in thin section.
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Transparency: |
Translucent
to Sub-Opaque
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Luster: |
Resinous,
Greasy, Silky, Waxy, Earthy
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Refractive
Index: |
1.555
- 1.573 Biaxial ( - )
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Birefringence: |
0.005
- 0.006
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Dispersion: |
Weak;
r > v
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Pleochroism: |
None
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Occurances
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Geological
Setting: |
Commonly
replaces ultramafic rocks, pervasively or in crosscutting
veinlets. As a replacement of siliceous dolostone along
contacts with diabase sills. |
Common
Associations: |
Chromite,
Chrysotile, Magnetite, Olivine |
Common
Impurities: |
Ni,
Al, Mn |
Co-Type
Localities: |
•
Antigorio Valley, Ossola Valley, Verbano-Cusio-Ossola Province, Piedmont, Italy;
• • Geisspfad area, Binn Valley, Wallis (Valais), Switzerland
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Year
Discovered: |
1840
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View
mineral photos: |
Antigorite
Mineral Photos and Locations |
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More
Information
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|
Mindat.org
Webmineral.com
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Antigorite
was named in 1840 by Mathias Eduard Schweizer for the type locality, Valle
di Antigorio, Domodossola, Piedmont, Italy; although there is some question whether
it was found on the Italian side or the Swiss side
of the border. Antigorite
is a member of the Serpentine
Group of minerals that
also includes Chrysotile
and
Lizardite. The
Serpentine Group is a subgroup of the Kaolinite-Serpentine Group.
Most Antigorite is opaque and fibrous but
a few locations produce beautiful, translucent, pale
to dark green material suitable for cabochons, carvings and
rarely faceted gems.
There
are a couple of gem varieties of Antigorite; Bowenite
and Williamsite.
Bowenite is a translucent, light green to dark
green, rarely blue-green, variety. Bowenite from China
is translucent and light yellowish green while Bowenite
from New Zealand can be dark green. Bowenite was named
by James D. Dana in 1850 for George T. Bowen, who first
analyzed the mineral from Rhode Island in 1822.
Williamsite
is a very
translucent, medium to deep, apple green variety of
Antigorite that gets its color from the presence of
chromium (Cr). It often has inclusions of black specks
and microcrystals of Chromite in
it. Williamsite
originally came from the historic State Line Chrome
Mine which lies just inside Lancaster County, Pennsylvania on
the Pennsylvania-Maryland border. Williamsite
was named by Charles Upham Shepard in 1848 in honor of its discoverer, Lewis
White Williams (1804-1873), a mineralogist and geologist of West Chester, Chester County,
Pennsylvania.
Sources
of Antigorite include the type locality; Antigorio Valley,
Piedmont, Italy; New South Wales, Australia; Tirol Austria;
Liaoning Province, China; Nagasaki and Fukuoka Prefectures,
Japan; Glen Urquhart, Scotland; and in the USA at Texas,
Pennsylvania; Baltimore, Maryland; and Brewster, New
York. Most of these locations produce opaque, fibrous material
not suitable for faceted gems or cabochons.
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Antigorite
gems for sale:
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Gem:
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Antigorite |
Stock
#:
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ANTIG-001 |
Weight:
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3.2050
ct |
Size: |
11.05
x 9.06 x 4.27 mm |
Shape: |
Oval
Cabochon |
Color: |
Pale
Green |
Clarity: |
Translucent |
Origin: |
China |
Treatment: |
None
(natural) |
Price: |
SOLD
(but we have others) |
Pictures
are of the actual gem offered for
sale. Gem images are magnified to
show detail. |
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A
beautiful pale green gem from China
with a high polish and glowing color.
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