Chemistry:Hoelite
From HandWiki
| Hoelite | |
|---|---|
 Yellow acicular crystals of hoelite (picture size: 10 mm) | |
| General | |
| Category | Organic mineral |
| Formula (repeating unit) | C14H8O2 |
| 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 | [1][2] |
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).[1]
It is a very rare organic mineral which occurs in coal fire environments in association with sal ammoniac and native sulfur.[1]
References
- ↑ 1.0 1.1 1.2 "Hoelite". Handbook of Mineralogy. Chantilly, VA: Mineralogical Society of America. http://www.handbookofmineralogy.com/pdfs/hoelite.pdf. Retrieved 12 September 2017.
- ↑ Barthelmy, Dave. "Hoelite". Mindat.org. https://www.mindat.org/min-1915.html. Retrieved 12 September 2017.
- ↑ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine 85 (3): 291–320. doi:10.1180/mgm.2021.43. Bibcode: 2021MinM...85..291W.
 |  |
