Spessartine Explained

Spessartine
Category:Nesosilicate
Garnet group
Formula:Mn2+3Al2(SiO4)3
Imasymbol:Sps[1]
Strunz:9.AD.25
System:Isometric
Class:Hexoctahedral (mm)
H-M symbol: (4/m 2/m)
Symmetry:Ia3d
Unit Cell:a = 11.63 Å; Z = 8
Color:Yellow through red
Habit:Massive to crystalline
Cleavage:None
Fracture:Sub-conchoidal
Tenacity:Brittle
Mohs:6.5 – 7.5
Luster:Vitreous
Refractive:1.800
Opticalprop:Isotropic, often anomalous double refractive
Birefringence:none
Dispersion:Weak
Absorption:Bands at 410, 420, 430 nm (or merging to form cutoff below 430 nm; also bands at 460, 480, 520 nm. Possible weak bands at 504 or 573 nm
Streak:White
Gravity:4.19 calculated, 4.12 – 4.32 measured
Diaphaneity:Transparent to translucent
References:[2] [3] [4]

Spessartine is a nesosilicate, manganese aluminium garnet species, Mn2+3Al2(SiO4)3.[5] [2] [3] [4] This mineral is sometimes mistakenly referred to as spessartite.[6]

Spessartine's name is a derivative of Spessart in Bavaria, Germany, the type locality of the mineral.[2] [3] It occurs most often in granite pegmatite[2] [3] [4] and allied rock types and in certain low-grade metamorphic phyllites. Sources include Australia, Myanmar, India, Afghanistan, Israel, Madagascar, Namibia, Nigeria, Mozambique, Tanzania and the United States.[5] Spessartine of an orange-yellow has been called Mandarin garnet and is found in Madagascar. Violet-red spessartines are found in rhyolites in Colorado and Maine. In Madagascar, spessartines are exploited either in their bedrock or in alluvium. The orange garnets result from sodium-rich pegmatites. Spessartines are found in bedrock in the highlands in the Sahatany valley. Those in alluvium are generally found in southern Madagascar or in the Maevatanana region.[7] [8] [9] [10] [11]

Spessartine forms a solid solution series with the garnet species almandine.[3] [4] Well-formed crystals from this series, varying in color from very dark-red to bright yellow-orange, were found in Latinka, Rhodope Mountains, Kardzhali Province, Bulgaria.[12] Spessartine, like the other garnets, always occurs as a blend with other species. Gems with high spessartine content tend toward a light orange hue, while almandine prevalence induces red or brownish hues.[13]

See also

Notes and References

  1. Warr. L.N.. 2021. IMA–CNMNC approved mineral symbols. Mineralogical Magazine. 85. 3. 291–320. 10.1180/mgm.2021.43. 2021MinM...85..291W. 235729616. free.
  2. http://www.webmineral.com/data/Spessartine.shtml Webmineral Spessartine page
  3. http://www.mindat.org/min-3725.html Mindat Spessartine page
  4. Web site: Handbook of Mineralogy Spessartine page . 2009-06-06 . 2016-03-04 . https://web.archive.org/web/20160304003406/http://www.handbookofmineralogy.com/pdfs/spessartine.pdf . dead .
  5. [Gemological Institute of America]
  6. International Mineralogical Association . 1971 . International Mineralogical Association: Commission on new minerals and mineral names . Mineralogical Magazine . 38 . 293 . 102–105 . 10.1180/minmag.1971.038.293.14. 1971MinM...38..102. .
  7. 1998-04-01. Gem News. Gems & Gemology. 34. 1. 50–63. 10.5741/GEMS.34.1.50. free.
  8. Shigley. James. Dona Dirlam . Brendan Laurs . Edward Boehm . George Bosshart . William Larson. 2000. Gem localities of the 1990s. Gems & Gemology. 36. 4. 292–335. 10.5741/GEMS.36.4.292. free.
  9. Laurs. Brendan. Kimberly Knox . 2001. Spessartine garnet from Ramona, San Diego County, California. Gems & Gemology. 37. 4. 278–295. 10.5741/GEMS.37.4.278. free.
  10. Rossman. George R.. 2009. The geochemistry of gems and its relevance to gemology: different traces, different prices. Elements. 5. 3. 159–162. 10.2113/gselements.5.3.159. 140651302. 1811-5209.
  11. Schmetzer. Karl. 2001 . Thomas Hainschwang . Lore Kiefert . Heinz-Jürgen Bernhardt. Pink to pinkish orange Malaya garnets from Bekily, Madagascar. Gems & Gemology. 37. 4. 296–308. 10.5741/GEMS.37.4.296. free.
  12. Web site: Spessartine from Latinka, Bulgaria.
  13. http://www.gemsociety.org/article/spessartite-garnet/ Spessartite Garnet Gemological Information