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| Jamesonite
is named to honor Robert Jameson (1774–1854), Scottish
mineralogist, Edinburgh, Scotland, who first described
the mineral.
| Discovered
in 1825.
IMA
status: Valid (pre-IMA; Grandfathered) |
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Chemistry
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Chemical
Formula: |
Pb4Fe2+Sb6S14
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Lead
Iron Antimony Sulfide |
Molecular
Weight: |
2,064.07 gm |
Composition: |
Iron |
2.71 % |
Fe |
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Antimony |
35.39 % |
Sb |
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Lead |
40.15 % |
Pb |
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Sulfur |
21.75 % |
O |
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100.00 % |
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Classification
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Mineral
Classification: |
Sulfides
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Strunz 8th
Ed. ID:
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2/E.22-10
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Nickel-Strunz 10th
Ed. ID:
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2.HB.15
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2 : SULFIDES and SULFOSALTS (sulfides, selenides,
tellurides; arsenides, antimonides, bismuthides; sulfarsenites,
sulfantimonites, sulfbismuthites, etc.) H : Sulfosalts of SnS archetype
B : With Cu, Ag, Fe, Sn and Pb
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Related
to: |
Benavidesite-Jamesonite
Series. Dimorphous with Parajamesonite.
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Synonyms: |
Axotomous Antimony Glance,
Comuccite, Cornuccite, Domingite, Jamesonite (of Haidinger),
Pfaffite (of Huot), Sakharovaite, Tinder Ore, Warrenite (of Eakins),
Wolfsbergite (of Huot)
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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
elongated || [001], acicular and fibrous, to 10
cm; striated k [001]; rarely in rings and spheres. As
feltlike masses; massive, columnar, also radial and
plumose.
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Twinning:
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On
{100}; lamellae very commonly observed in polished section.
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Physical
Properties
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Cleavage: |
Good
on {001}; reported on {010} and {120}
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Fracture: |
n/a
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Tenacity:
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Brittle
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Moh's
Hardness: |
2.5;
VHN = 66–86 (100 g load)
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Density:
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5.63 (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: |
Gray-Black,
lead Gray, Steel Gray, dark lead Gray; iridescent at times
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Transparency: |
Opaque
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Luster: |
Metallic
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Refractive
Index: |
R1–R2:
(400) 38.4–45.1, (420) 38.1–44.9, (440) 37.7–44.8, (460)
37.6–45.0, (480) 37.4–45.1, (500) 37.3–45.0, (520) 37.0–44.7,
(540) 36.6–44.3, (560) 36.1–43.8, (580) 35.7–43.2, (600)
35.3–42.6, (620) 34.8–41.9, (640) 34.2–41.0, (660) 33.6–40.1,
(680) 33.0–39.2, (700) 32.5–38.5
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Pleochroism: |
Distinct
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Anisotrophism: |
Strong; Color in reflected light:
Gray-Black
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Occurances
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Geological
Setting: |
Typically
a late-stage hydrothermal mineral in Pb–Ag–Zn veins
formed at low to medium temperatures. |
Common
Associations: |
Other
lead Sulfosalts, Pyrite, Sphalerite, Galena, Tetrahedrite,
Stibnite, Quartz, Siderite, Calcite, Dolomite, Rhodochrosite.
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Common
Impurities: |
Cu,
Zn, Ag, Bi |
Type
Locality: |
Cornwall, England, UK
|
Year
Discovered: |
1825
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View
mineral photos: |
Jamesonite
Mineral Photos and Locations |
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More
Information
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Mindat.org
Webmineral.com
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Jamesonite
is one of a few sulfide minerals that form fine acicular
crystals that appear as hair-like fibers.
Jamesonite also forms larger prismatic crystals that can be confused with Stibnite.
Jamesonite has been called feather ore and gray antimony.
Jamesonite is rarely available as inclusions in Quartz cabochons.
This material is available from Minas Gerais, Brazil.
Jamesonite
is available from numerous localities, but only a few
have provided rich material. From Cornwall, England,
around St. Endellion [TL] and St. Kew. In Germany, at
Freiberg, Saxony; and near Magdesprung, Selke Valley,
and Clausthal, Harz Mountains. From Príbram, Czech Republic.
At Aranyidka, Baia Sprie (Felsöbánya), and Herja (Kisbánya),
Baia Mare (Nagybánya) district, Romania. From Trepca,
Serbia. At Sala, Västmanland, Sweden. From Machacamarca,
Poopó, and Huanuni, Oruro, Bolivia. In Mexico, from
the Noche Buena mine, near Mazapil; the Santa Rita mine,
Nieves; and in relatively thick crystals from the Noria
mine, near Sombrerete, Zacatecas. In the USA, in Idaho,
at Slate Creek, Shoshone County From the Dachang district,
Guangxi Autonomous Region, China.
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Jamesonite
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