Spessartine (variety of Garnet)
Current inventory:  0 gems
 

  
Spessartine is named after the Spessart Mts, Germany where it was discovered.

Discovered in 1832; IMA status: Valid (pre-IMA; Grandfathered)

Chemistry

Chemical Formula:

Mn²⁺₃Al₂(SiO₄)

Manganese Aluminum Silicate

Molecular Weight:

495.03 gm

Composition:

Manganese

33.29 %

Mn

42.99 %

MnO

Aluminum

10.90 %

Al

20.60 %

Al₂O₃

Silicon

17.02 %

Si

36.41 %

SiO₂

Oxygen

38.78 %

O

100.00 %

100.00 %

= TOTAL OXIDE

Classification

Mineral Classification:

Silicates (Germanates)

Strunz 8th Ed. ID:

8/A.08-30

Nickel-Strunz 10th Ed. ID:

9.AD.25

9 : SILICATES (Germanates)
A : Nesosilicates
D : Nesosilicates without additional anions; cations in [6] and/or greater coordination

Related to:

Garnet Group. Almandine-Spessartine Series.

Members of Group:

Garnet Group: Almandine, Andradite, Grossular, Pyrope, Spessartine, Uvarovite

Varieties:

Brandãosite, Calcium-Eisenspessartin, Emildine, Spandite

Synonyms:

Erinite (of van der Lingen), Mandarin Garnet, Partschinite, Spessartine Garnet, Spessartite

Crystal Data

Crystallography:

Isometric - Hexoctahedral

Crystal Habit:

Commonly as euhedral crystals, dodecahedra or trapezohedra, or in combination with other cubic forms, to 10 cm. Fine or coarse granular, compact, massive.

Twinning:

None

Physical Properties

Cleavage:

None (?)

Fracture:

Irregular/Uneven to Conchoidal

Tenacity:

Brittle

Moh's Hardness:

7.0 - 7.5

Density:

4.190 (g/cm³)

Luminescence:

None

Radioactivity:

Not Radioactive

Optical Properties

Color:

Red, reddish orange, yellow, yellowish brown, reddish brown, brown, black; pale pink to pale brown in thin section, may be sectored.

Transparency:

Transparent to Translucent

Luster:

Vitreous

Refractive Index:

1.800 Isotropic

Birefringence:

0.000 (Isotropic)

Dispersion:

Weak

Pleochroism:

None

Anisotrophism:

May show weak anisotropism.

Occurances

Geological Setting:

Common in granite pegmatites, granites, and rhyolites. Formed in some skarns and metasomatic manganese-rich rocks adjacent to igneous intrusions or in regionally metasomatized areas.

Common Associations:

Quartz, Potassic Feldspar, Tourmaline, Rhodonite, Pyroxmangite, Tephroite, Alleghanyite, Galaxite, Muscovite, Topaz, Apatite, Beryl, Albite, Bixbyite, Pseudobrookite.

Common Impurities:

None

Type Locality:

Sommer quarry, Wendelberg, Haibach, Aschaffenburg, Spessart, Franconia, Bavaria, Germany

Year Discovered:

1832

View mineral photos:

Spessartine Mineral Photos and Locations

More Information

Mindat.org
Webmineral.com

Spessartine, also called Spessartite, is a member of the Garnet Group of minerals that includes Almandine, Andradite, Grossular, Pyrope, Spessartine and Uvarovite. Spessartine is fairly rare as a gem Garnet, and one of the most beautiful. Large gems are very rare and usually quite dark. The finest color is an orangy red, as exemplified by material from Ramona, California, USA and Amelia, Virginia, USA. A red-brown tint indicates a higher content of Almandine, accompanied by a higher refractive index; pale to bright orange colors are closer to pure Spessartine. Bright orange Spessartine Garnets are often called Mandarin Garnets. Spessartine as a component of Almandine gems tends to add a lively reddish tinge of color.

Rare color change Garnets with large amounts of  vanadium (V) and chromium (Cr) have been reported from East Africa. These are primarily Spessartine, with an unusually large component of Grossular. There are generally two types of color change displayed: either greenish yellow-brown in fluorescent light to purplish red or reddish orange in incandescent light; or light bluish green in fluorescent light to purplish red or red in incandescent light. So-called Alexandrite-like Garnets are also found from Bekily, Madagascar. These gems display a distinct color change from violet-red to blue-green.

Spessartine, like other garnets, forms rounded crystals with 12 rhombic or 24 trapezoidal faces or combinations of these and some other forms. This crystal habit is classic for the Garnet minerals. Spessartine is formed in manganese rich metamorphic environments and in some granitic pegmatites.

Distribution: While a less-common garnet, nevertheless many localities. From Aschaffenburg, Spessart Mountains, Bavaria, Germany. On Seriphos, Cyclades Islands, Greece. In the USA, in Leiper's quarry, Avondale, Delaware County, Pennsylvania; the Rutherford mine, Amelia, Amelia County, Virginia; in the Ramona and Pala districts, San Diego County, California; from the Thomas Range, Juab County, Utah; at Ely, White Pine County, Nevada; from near Nathrop, Chaffee County, Colorado. In Brazil, from Nangue and Urucum, Minas Gerais, and at Carnaúba, near Picui, Rio Grande do Norte. From Marienflüss, Namibia. At Tsilaizina and Anjanabonoina, Madagascar. In the Gilgit district, and at Dusso, Baltistan, Pakistan. From Broken Hill, New South Wales, Australia. At Wada-toge Pass, Nagano Prefecture, Japan.
 

  
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