| Putnisite | |
| Formula: | SrCa4Cr83+(CO3)8(SO4)(OH)16·25 H2O |
| Imasymbol: | Pni[1] |
| Class: | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
| Symmetry: | Pnma |
| Unit Cell: | a = 15.351 Å, b = 20.421 Å, c = 18.270 Å; Z = 4 |
| Color: | Purple |
| Habit: | Pseudocubic crystals |
| Cleavage: | [100], [010] and [001] good |
| Fracture: | Brittle – uneven |
| Mohs: | 1.5–2 |
| Luster: | Vitreous |
| Refractive: | nα = 1.552, nβ = 1.583 and nγ = 1.599 |
| Opticalprop: | Biaxial (−) |
| Pleochroism: | Distinct: X pale bluish grey, Y pale purple, Z pale purple |
| Streak: | Pink |
| Gravity: | 2.20 |
| Diaphaneity: | Translucent |
| References: | [2] [3] [4] [5] |
Putnisite is a mineral composed of strontium, calcium, chromium, sulfur, carbon, oxygen and hydrogen.[4] It was discovered on the Polar Bear Peninsula in Shire of Dundas, Western Australia in 2007 during mining activity.[4] [5] Following identification and recognition by the IMA in 2012[5] the mineral was named after mineralogists Andrew and Christine Putnis.[3]
Putnisite has unique chemical and structural properties, and does not appear to be related to any of the existing mineralogical families.[3] Crystals are translucent purple, but show distinct pleochroism (from pale purple to pale bluish grey,[4] depending on the angle of observation) and leave pink streaks when rubbed on a flat surface.[4]
Putnisite occurs as small (< 0.5 mm) cube-like crystals in volcanic rock.[3] The mineral formed during the oxidation environment within komatiite to dioritic bodies containing sulfide minerals.[4]