| Mendozite | |
| Category: | Sulfate minerals, alum series |
| Formula: | NaAl(SO4)2·11H2O |
| Imasymbol: | Mz[1] |
| Molweight: | 440.26 g/mol |
| Strunz: | 7.CC.15 |
| Dana: | 29.5.4.1 |
| System: | Monoclinic |
| Class: | Prismatic (2/m) (same H-M symbol) |
| Symmetry: | C2/c |
| Color: | colorless |
| Habit: | prismatic, pseudo-rhombohedral |
| Cleavage: | good indistinct indistinct |
| Mohs: | 3 |
| Luster: | vitreous |
| Streak: | white |
| Diaphaneity: | transparent to translucent |
| Density: | 1.74 g/cm3 |
| Refractive: | nα = 1.449 nβ = 1.461 nγ = 1.463 |
| Opticalprop: | biaxial (-) |
| Birefringence: | δ = 0.014 |
| 2V: | 56° (measured) |
| Solubility: | soluble in water |
| Alteration: | tamarugite |
| References: | [2] [3] [4] [5] |
Mendozite is a sulfate mineral, one of the alum series, with formula NaAl(SO4)2·11H2O. It is a hydrated form of sodium aluminium sulfate (soda alum).
It was discovered in western Argentina in 1868, probably near San Juan. The exact location has been lost, but was described as "San Juan, near Mendoza", and it is the latter city that give the mineral its name.[3] It occurs in evaporites, presumably from the oxidation of sulfide minerals in the presence of clays.[3] It is very soluble in water, and so can only be found in dry regions: however, in can still effloresce (lose water of crystallisation) in extremely arid climates, altering to tamarugite (the hexahydrate).[4]