| Hoelite | |
|---|---|
|  Yellow acicular crystals of Hoelite (picture size: 10 mm) | |
| General | |
| Category | Organic mineral | 
| Formula (repeating unit) | C14H8O2 | 
| IMA symbol | Hoe[1] | 
| Strunz classification | 10.CA.15 | 
| Dana classification | 50.4.2.1 | 
| Crystal system | Monoclinic | 
| Crystal class | Prismatic (2/m) (same H-M symbol) | 
| Space group | P21/a | 
| Unit cell | a = 15.81 Å, b = 3.967 Å c = 7.876 Å; β = 102.67°; Z = 2 | 
| Identification | |
| Color | Yellow, yellowish green | 
| Crystal habit | Acicular clusters; pseudo-orthorhombic | 
| Cleavage | Good | 
| Streak | Light yellow | 
| Diaphaneity | Semitransparent | 
| Specific gravity | 1.42 | 
| Optical properties | Biaxial (+) | 
| Refractive index | nα≈1.75, nβ≈1.75, nγ≈2.0 | 
| References | [2][3] | 
Hoelite is a mineral, discovered in 1922 at Mt. Pyramide, Spitsbergen, Norway and named after Norwegian geologist Adolf Hoel (1879–1964). Its chemical formula is C14H8O2 (9,10-anthraquinone).[2]
It is a very rare organic mineral which occurs in coal fire environments in association with sal ammoniac and native sulfur.[2]
References

Wikimedia Commons has media related to Hoelite.
- ↑ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- 1 2 3 Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C. (eds.). "Hoelite" (PDF). Handbook of Mineralogy. Chantilly, VA: Mineralogical Society of America. Retrieved 12 September 2017.
- ↑ Barthelmy, Dave. "Hoelite". Mindat.org. Retrieved 12 September 2017.
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