thorite
{{Short description|Nesosilicate mineral}}
{{infobox mineral
|boxbgcolor=#926339| name = Thorite
| boxtextcolor = #fff
| image = Thorite-288916.jpg
| imagesize = 260px
| caption = Thorite crystal from the Kemp uranium mine in Ontario (size: 2.2 x 2.2 x 1.6 cm)
| category = Silicate mineral
| formula = (Th,U)SiO4
| molweight =
| strunz = 9.AD.30
| dana =
| system = Tetragonal
| class = Ditetragonal dipyramidal (4/mmm)
H-M symbol: (4/m 2/m 2/m)
| symmetry = I41/amd
| unit cell = a = 7.13, c = 6.32 [Å]; Z = 4
| color = Yellow-orange, brownish yellow, brownish black, black, green
| colour =
| habit = In square prisms, or pseudo-octahedral crystals; also massive
| twinning =
| cleavage = Distinct on {110}
| fracture = Conchoidal
| tenacity = Brittle
| mohs = 4.5 – 5
| luster = Vitreous to resinous
| streak = Light orange to light brown sometimes even an alien magenta
| diaphaneity = Nearly opaque, transparent in thin fragments
| gravity = 6.63 – 7.20
| density =
| polish =
| opticalprop = Uniaxial (−)
| refractive = nω = 1.790 – 1.840 nε = 1.780 – 1.820
| birefringence = δ = 0.010 – 0.020
| pleochroism =
| 2V =
| dispersion =
| extinction =
| length fast/slow =
| fluorescence =
| absorption =
| melt =
| fusibility =
| diagnostic =
| solubility =
| impurities =
| alteration = Commonly metamict
| other = 25px Radioactive
| prop1 =
| prop1text =
| references = [http://webmineral.com/data/Thorite.shtml Webmineral data][http://www.mindat.org/min-3946.html Mindat.org][http://rruff.geo.arizona.edu/doclib/hom/thorite.pdf Handbook of Mineralogy]
}}
Thorite, (Th,U)SiO4, is a rare nesosilicate of thorium that crystallizes in the tetragonal system and is isomorphous with zircon and hafnon. It is the most common mineral of thorium and is nearly always strongly radioactive. Thorite was discovered in 1828 on the island of Løvøya, Norway, by the vicar and mineralogist, Hans Morten Thrane Esmark. First specimens of Thorite were sent to his father, Jens Esmark, who was a professor of mineralogy and geology.{{cite journal | doi = 10.1080/14786442908675174 | title = Thorite, a new mineral, and thorina, a new earth | year = 1829 | last1 = Berzelius | first1 = M. | journal = Philosophical Magazine |series=Series 2 | volume = 6 | issue = 35 | pages = 392–393| url = https://zenodo.org/record/1430987 }}{{cite journal | doi = 10.1002/andp.18290920702 | title = Untersuchung eines neuen Minerals und einer darin enthaltenen zuvor unbekannten Erde | year = 1829 | last1 = Berzelius | first1 = J. J. | journal = Annalen der Physik und Chemie | volume = 92 | issue = 7 | pages = 385–415 |bibcode = 1829AnP....92..385B | url = https://zenodo.org/record/1423530 }}{{cite journal | last1 = Marshall | first1 = J.L. | last2 = Marshall | first2 = V.R. | year = 2001 | title = Rediscovery of the Elements- Thorium-Løvøya, Langesundsfjord, Norway | journal = The Hexagon | volume = 93 | pages = 70–73 | url = http://www.chem.unt.edu/Rediscovery/Thorium.pdf | url-status = dead | archiveurl = https://web.archive.org/web/20050408114055/http://www.chem.unt.edu/Rediscovery/Thorium.pdf | archivedate = 2005-04-08 }}
It was named in 1829 to reflect its thorium content.
Occurrence
File:Thorites - CAMR www.amrminerals.co.uk 10-crop.jpg
Specimens of thorite generally come from igneous pegmatites and volcanic extrusive rocks, hydrothermal veins and contact metamorphic rocks. It is also known to occur as small grains in detrital sands. Crystals are rare, but when found can produce nicely shaped short prismatic crystals with pyramidal terminations.
It is commonly associated with zircon, monazite, gadolinite, fergusonite, uraninite, yttrialite and pyrochlore.
Thorite is currently an important ore of uranium. A variety of thorite, often called "uranothorite", is particularly rich in uranium and has been a viable uranium ore at Bancroft in Ontario, Canada. Other varieties of thorite include "orangite", an orange variety, and "calciothorite", an impure variety with trace amounts of calcium.
Properties
Due to the radioactive elements contained, Thorite is commonly metamict. With the destructive effects of radioactivity on the crystal lattice, hydrated specimens are often amorphous and optically isotropic.
Owing to differences in composition, the specific gravity varies from 4.4 to 6.6 g/cm3. Hardness is 4.5 and the luster is vitreous or resinous. The color is normally black, but can range from brownish black to orange, yellowish-orange and dark green.
References
{{Reflist}}
External links
{{Commons category|Thorite}}
{{EB1911 poster|Thorite}}
Category:Radioactive gemstones