Zircon from Seiland, Norway.
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A 2 cm zircon crystal in biotite, from Seiland, Norway.
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Zircon and albite on orthoclase, from Langesundsfjorden, Norway.
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Zircon in feldspar, from Langesundsfjorden, Norway.
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| Mineral class | Silicates : Nesosilicates : Zircon - tantalite group. |
| Chemical formula | Zr(SiO4) |
| Crystal system | Tetragonal |
| Habitus | Short prismatic dipyramidal crystals or irregular grains. |
| Cleavage | Imperfect, uneven to conchoidal fracture. |
| Hardness | 7.5 |
| Density | 4.6-4.7 |
| Color | Colorless, red, brown, yellow, green or gray. Transparent to opaque. |
| Streak |   |
| Luster | Vitreous, adamantine to greasy. |
| Description |   |
| Occurance | In granites, pegmatites and nefeline syenites. |
| Associates |   |
| Notes | Often radioactive due to small amounts of thorium and uranium.
(Up to 14 %) Zircon is often metamict (no crystal structure) because of the radioactivity thats destroyed the internal structure. Zircon is a very good mineral to measure the age of rocks. It encapsules the uranium and the rest product, led, so it is possible to measure the age of different layers in a zircon crystal. The oldest zircon found in Sweden is 3300 million years old. Flourescent in UV-light. |
| Locations | A common mineral in microscopic amounts.
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| To silicate index. |
Mineral group index. |
Main index. |
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