Mineral Name Torbernite
First Discovered 1772
Nickel-Strunz Classification 08.EB.05
Dana Classification 40.02a.13.01
ICSD Pre IMA
Mineral Group Phosphates

 

Torbernite is a radioactive mineral that was named after Torbern Olof Bergmann (1735-1784). Tobernite was first discovered in 1772 in Cechy (Bohemia), Czech Republic. As a radioactive mineral, torbernite has some limited significance as a uranium ore. Its rich green colour and well-developed distinctive crystals make it a sought-after collector's mineral, as well. However, torbernite, like other hydrated minerals, can easily suffer from loss of water molecules. This loss of water from the mineral leads to an alteration of torbernite specimens into its pseudo morph, meta-torbernite.

Torbern Olof Bergman (March 20, 1735 Katrineberg, Sweden, – July 8, 1784 Medevi, Sweden) was a Swedish chemist and mineralogist noted for his 1775 Dissertation on Elective Attractions, containing the largest chemical affinity tables ever published. Bergman was the first chemist to use the A, B, C, etc., system of notation for chemical species.

 

Within the metaphysical realm of minerals, torbernite is a harmful mineral and should not be handled for prolonged periods of time. Please check out the 'Health Hazards' section of this article for more information.

Please note that MIROFOSS does not suggest in any way that minerals should be used in place of proper medical and psychological care. This information is provided here as a reference only.

Torbernite is mined as a minor ore of uranium. Torbernite is also sought after by collectors however, special precautions should be taken if this mineral is to be placed on display.

Torbernite is a secondary mineral in granites, and other uranium-bearing rocks. Torbernite can also be found in the oxidized zones of some uraniferous copper deposits.

Due to the fact that torbernite is radioactive, mineral samples will give off radon gas which is a major contributor to lung cancer.  To protect living beings from radon gas, a method of sealed storage can be used in which radon will accumulate and decay to secular equilibrium.

Cleavage Perfect to Distinct
Colour(s) Green, Grass green, Siskin green, Apple green
Specific Gravity 3.20
Diaphaneity Transparent to Sub transparent
Fracture Brittle - generally displayed by glasses and other non-metallic minerals
Mohs Hardness 2.0 to 2.5
Luminescence Short UV = yellow, Long UV = yellow
Lustre Vitreous - pearly
Streak Pale green
Habit(s) Earthly to Tabular to Foliated
Radioactivity Torbernite per GRadi unit = 269.90 (PPB)
Magnetism Non-magnetic

The following health hazards should be noted when handling torbernite

RADIOACTIVE

Torbernite is radioactive as defined in section 49 CFR 173.403. Greater than 70 Bq / gram.
Torbernite is considered extremely radioactive.


The following image shows the Elemental breakdown of the mineral torbernite along with the mineral crystal structure.

Crystal System Tetragonal
Class Ditetragonal Dipyramidal
Axial Ratios a : b : c = 1 : N/A : 2.90934
Morphology Commonly forms sub parallel aggregates, foliated, micaceous, scaly
Optical Data Type Uniaxial (-)
Dichroism (e) Blue
Dichroism (w) Green
Pleochroism Visible
RL Values nω = 1.590 - 1.592 nε = 1.581 - 1.582
2V Measured: 8°
Max Birefringence δ = 0.009 - 0.010(See colour chart at right)
Surface Relief moderate
   

Torbernite can be referenced in certain current and historical texts under the following eight names:


The mineral torbernite can be translated into the following select languages:
Arabic   Bulgarian   Chinese (Sim) 铜铀云母
Croatian   Czech torbernit Danish  
Dutch Torberniet Esperanto   Estonian  
Finnish   French Urane oxydé German Torbernit
Greek   Hebrew   Hungarian  
Italian Torbernite Japanese トルボルナイト Korean 토부루나입
Latin Uranites Spathosus Lithuanian   Norwegian  
Persian   Polish   Portuguese Torbernite
Romanian   Russian   Slovak Torbernit
Spanish Torbernita Swedish   Tagalog  
Turkish   Ukrainian   Vietnamese  

Torbernite can be found in a few places around the world. The map below shows major documented concentrations of torbernite:

The MIROFOSS database offers free printable geological identification tags for personal and non-profit use. These tags can be used to properly identify mineral samples in your collection. -Click here- to download a full size jpeg image for a torbernite identification tag; which can be printed on paper or used with a plastic laser printer.

What's this?
This is a QR code (short for Quick Response) which gives fast-track access to MIROFOSS articles. QR Codes are barcodes that can be read by smart phone cameras. This QR Code is unique to this MIROFOSS article.

What can I do with it?
You can copy and print the QR code to a plant label, poster, book, web site, magazines, or newspaper so smart phone users can scan the QR Code which automatically takes them to this specific article.

Chemical Composition Aikin, A. (1814) Manual of Mineralogy, 8 volumes, London, first edition (as Uranite).
Chemical Composition Burns, P.C. (2005) U 6+ minerals and inorganic compounds: insights into an expanded structural hierarchy of crystal structures. Canadian Mineralogist: 43: 1839-1894.
Crystallography Jameson, R. (1820) A System of Mineralogy, third edition, 3 volumes (as Uran-Mica).
Crystallography Larsen, E.S. (1921) The Microscopic Determination of the Nonopaque Minerals, First edition, USGS Bulletin 679: 195.
History Brooke, H.J. and Miller, W.H. (1852) Introduction to Mineralogy by Wm. Phillips, London, 1823. New edition by Brooke and Miller. 8vo, London: 517 (as Torberite).
History Dana, E.S. (1892) System of Mineralogy, 6th. Edition, New York: 856.
Geograpcial Data Mindat.org. Retrieved on 2012-02-21
Physical Identification Webmineral.com. Retrieved on 2012-02-21.
February 21, 2012 The last time this page was updated
©2017 MIROFOSS™ Foundation