Euxenite from Godkärra.Two small samples. |
Euxenite crystal from Godkärra.
The crystal is the dark grain in the top border.
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Euxenite from Godkärra.
In feldspar, showing radiation damage. |
| Mineral class | Oxides : Perovskite - Pyrochlore - Columbite group. |
| Chemical formula | (Y,Er,Ce,U,Pb,Ca)(Nb,Ta,Ti)2(O,OH)6 |
| Crystal system | Orthorombic. |
| Habitus | As short thick prismatic crystals. Also as derb masses. |
| Cleavage | None, fracture brittle conchoidal. |
| Hardness | 5.5-6.5 |
| Density | 4.3-5.9 |
| Color | Dark brown to black. |
| Streak | Light brown. |
| Luster | Metallic to vitreous. |
| Description | A radioactive mineral, sometimes used as an ore of tantalum, terbium, Thulium. |
| Occurance | In granitic pegmatites. |
| Associates | Quartz, feldspar, columbite, tantalite, monazite. |
| Notes | Radioactive. Historial fact : Euxenite played an important role in the discovery of scandium, the 21:st element in the periodic system. (L. Scandia, Scandinavia) On the basis of the Periodic System, Mendeleev predicted the existence of ekaboron in 1871, which would have an atomic weight between 40 of calcium and 48 of titanium. The element was later discovered by Lars Nilson in 1878 in the minerals euxenite and gadolinite, which had not yet been found anywhere except in Scandinavia. By processing 10 kg of euxenite and other residues of rare-earth minerals, Nilson was able to prepare about 2g of highly pure scandium oxide. Later scientists pointed out that Nilson's scandium was identical with Mendeleev's ekaboron. Euxenite was first described in 1870 by Scheerer. Origin of name : From the Greek eu - "good" and xenos - "foreigner." |
| Locations | A relatively rare mineral in Sweden.
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| To oxides index. |
Mineral group index. |
Main index. |
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