Uranocircite |
IMA-GP |
| Uranium | 40.2a.3.1 (Dana Classification Number) |
| (Images) | 7/E.01-110 (Strunz ID) |
| Unless sealed in glass, all specimens should be considered to have become Meta-Uranocircite within a few months of being exposed to ambient air. | |
| Property | Data | Remarks | ||||||||||||||||||||
| Named for: | Its composition, and the Greek for falcon - refering to Falkenstein, Saxony, Germany, where it is commonly found | |||||||||||||||||||||
| Alternate Name(s): |
||||||||||||||||||||||
| Mineral Class: |
|
|||||||||||||||||||||
| Chemical Formula: |
Ba(UO2)2(PO4)2 · 10-12H2O | |||||||||||||||||||||
| Chemical Composition: |
|
by weight | ||||||||||||||||||||
| Molecular Weight: |
1,083.51 | daltons (amu) | ||||||||||||||||||||
| Specific Radioactivity: |
(All radiation is for a 1 gram, fully aged specimen)
Estimated Average Annual Exposure: 360 mRem (3.6 milliSieverts) |
|||||||||||||||||||||
| Crystalography: |
|
|||||||||||||||||||||
| Habit: |
|
|||||||||||||||||||||
| Cleavage: |
Cleavage sheets are slightly bendable. |
|||||||||||||||||||||
| Fracture: | Uneven, flexible | |||||||||||||||||||||
| Moh's Hardness: |
2 - 2.5 | |||||||||||||||||||||
| Density: | 3.46 - 3.53 | grams/cm3 | ||||||||||||||||||||
| Color: | Yellow to light Yellow-green | |||||||||||||||||||||
| Streak: | Light yellow | |||||||||||||||||||||
| Luster: | Vitreous, to Pearly on the main pinacoid | |||||||||||||||||||||
| Diaphaneity: | Transparent | |||||||||||||||||||||
| Pleochroism: |
|
|||||||||||||||||||||
| Ultra Violet Fluorescence: |
|
|||||||||||||||||||||
| Magnetism: | Non-magnetic | |||||||||||||||||||||
| Occurance: |
|
|||||||||||||||||||||
| Associated Minerals: |
Arsenopyrite, Autunite, Barite, Calcite, Chalcopyrite, Dewindtite, Fluorite, Galena, Hematite, Kasolite, Marcasite, Meta-Autunite, Parsonsite, Phosphuranylite, Pyrite, Pyrrhotite, Quartz, Sabugalite, Safflorite, Torbernite, Uraninite, Pitchblende, Uranophane, Uranopilite
|
These are minerals known to be found with Uranocircite | ||||||||||||||||||||
| Locations: | Relatively common Uranocircite Locations |
|||||||||||||||||||||
| Notes: | Very radioactive a- and b-particles, g-rays. Uranocircite can be difficult to distinguish from Autunite by ordinary means. However, Uranocircite is slightly heavier, its color is usually more yellow, and its fluorescent color is more green. Uranocircite can lose water and convert to a different mineral called meta-Uranocircite of the meta-autunite/meta-torbernite group of minerals. The change to meta-Uranocircite will often produce a pseudomorph. Crystals are probably metamict. |
|||||||||||||||||||||
| Image courtesy of The Arkenstone ![]() |
|||
| Malacacheta, Minas Gerais, Brazil | |||
![]() |
![]() |
||
| Bergen, Falkenstein, Vogtland, Saxony, Germany | |||