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Garnet Group: Spessartite & Mandarin Garnet



THE GARNET GROUP
  
Almandine   |  Andradite   |  Grossularite (Tsavorite)   |  Pyrope Garnet
Spessartite (Mandarin Garnet)   |  Uvarovite

Spessartite (Spessartine)


Spessartite Mandarin Garnet


Source: Australia, Brazil, Burma, Madagascar, Mozambique, Namibia, Nigeria, Sri Lanka, Tanzania, USA


Spessartite garnet, also known as spessartine, was named for its original location of discovery in the Spessart mountains of northwestern Bavaria in 1832. Spessartine is classified as a nesosilicate manganese aluminium garnet, in the silicate mineral group.



The "garnet group" is divided into six common varieties that are identified by their chemical composition and/or distinct color. The six main garnet types are almandine, andradite, grossularite, pyrope, spessartite, and uvarovite.


Spessartite Composition & Geology

Spessartine commonly occurs within metamorphic rock, and in ultramafic igneous rock formations, granite pegmatite, and low-grade metamorphic phyllites. The major sources for gem-grade orange spessartine are Brazil and Sri Lanka, with a violet-red variety occurring in the USA (Colorado).



Spessartine from Tanzania

Spessartine from Tanzania (© Swala Gem Traders)

   Mandarin Garnet from Namibia

Mandarin Garnet from Namibia (© Swala Gem Traders)


Spessartite was also mined in East Africa at Archer's Post, Kenya in the early 1900s, and more recently in Tanzania's Umba River Valley near the Kenya-Tanzania border, in northern Mozambique, and near the Serengeti National Park in northern Tanzania.


Mandarin Garnet

Mandarin Garnet is an extremely rare variety of garnet, and very recent mineral discovery, having been first identified in 1991. Mandarin Garnet, also known as Kunene spessartines, is a manganese (Mn) aluminium (Al) variety of garnet with an intense, and deeply saturated ideochromatic hue of pure-orange to yellowish-orange (above, right).


Garnet Crystal Structure

Since its discovery, the primary source for Mandarin Garnet has been the alluvial secondary deposits along the Kunene River between Namibia and Angola, in southwestern Africa. In recent years this primary source appears to be mined out, and new sources for Mandarin Garnet have been identified in south-western Nigeria in 1994, and more recently in Madagascar and Sri Lanka.



Spessartite specimens from Nigeria have a more reddish-orange hue, while the specimens from Madagascar and Sri Lanka are more of an orange-red with brownish overtones.


Spessartite Garnet & Tsavorite Chemistry, Physical Properties

Crystal System isometric (rhombic dodecahedron)
Crystal Habit massive and granular
Specific gravity (SG) 4.14 to 4.20
Mohs Hardness Scale 7.0 to 7.5
Toughness fair to good
Fracture conchoidal
Cleavage absent
Streak white
Associated Minerals granite, gneiss, marble, pegmatite
Chemical Composition Mn3Al2(SiO4)3

Spessartite (Mandarin) Garnet & Tsavorite Optical Properties

Optical Properties singly refractive
Refractive Index 1.79 - 1.81
Birefringence none
Pleochroism monochroic
Surface Luster vitreous to resinous
Diaphaneity transparent to translucent
Gem Color brown, orange, reddish-orange, yellowish-orange





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Bibliography on Spessartine & Mandarin Garnet


Swala Gem Traders, Spessartite Discovery in Northern Tanzania . www.swalagemtraders.com

ICA, Mandarin Garnet . www.gemstone.org




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