Tyuyamunite |
IMA-GP |
| Uranium | 40.2a.26.1 (Dana Classification Number) |
| (No Images) | 7/E.11-80 (Strunz ID) |
| Unless sealed in glass, all specimens should be considered to have become Metatyuyamunite within a few months of being exposed to ambient air. | |
| Property | Data | Remarks | ||||||||||||||||||||
| Named for: | Tyuya Muyun hill (Tuja Mujun) (a northern spur of the Alai Mountains), Ferghana, Uzbekistan, its type locality | |||||||||||||||||||||
| Alternate Name(s): |
||||||||||||||||||||||
| Mineral Class: |
|
|||||||||||||||||||||
| Chemical Formula: |
Ca(UO2)2(VO4)2 · 5-8H2O | |||||||||||||||||||||
| Chemical Composition: |
|
by weight | ||||||||||||||||||||
| Molecular Weight: |
918.10 | daltons (amu) | ||||||||||||||||||||
| Specific Radioactivity: |
(All radiation is for a 1 gram, fully aged specimen)
Estimated Average Annual Exposure: 360 mRem (3.6 milliSieverts) |
|||||||||||||||||||||
| Crystalography: |
|
Tyuyamunite Crystal |
||||||||||||||||||||
| Habit: |
|
|||||||||||||||||||||
| Cleavage: |
|
|||||||||||||||||||||
| Fracture: | Uneven | |||||||||||||||||||||
| Moh's Hardness: |
1.5 - 2 | |||||||||||||||||||||
| Density: | 3.3 - 3.8 - 4.3 (higher density with lower water content) |
grams/cm3 | ||||||||||||||||||||
| Color: | Yellow | |||||||||||||||||||||
| Streak: | Light yellow to Greenish yellow | |||||||||||||||||||||
| Luster: | Adamantine - Pearly | |||||||||||||||||||||
| Diaphaneity: | Translucent to Opaque | |||||||||||||||||||||
| Pleochroism: |
|
|||||||||||||||||||||
| Ultra Violet Fluorescence: |
|
|||||||||||||||||||||
| Magnetism: | Non-magnetic | |||||||||||||||||||||
| Occurance: |
|
|||||||||||||||||||||
| Associated Minerals: |
Autunite, Barite, Calcite, Carnotite, Coffinite, Huemulite, Malachite, Metatyuyamunite, Pyrite, Quartz, Schröckingerite, Uraninite, Uranophane
|
These are minerals known to be found with Tyuyamunite | ||||||||||||||||||||
| Locations: | Relatively common Uranium mineral Tyuyamunite Locations |
|||||||||||||||||||||
| Notes: | Strongly radioactive a- and b-particles, g-rays. Crystal structure is the single best way to differentiate it from Carnotite. |
|||||||||||||||||||||