Glauberite
Chemical formula: Na<sub>2</sub>Ca(S<sup>6+</sup>O<sub>4</sub>)<sub>2</sub>
Glauberite is a sulfate mineral, a double sulfate of sodium and calcium, often forming tabular crystals.
Properties
- Mohs hardness
- 2.5-3
- Luster
- Vitreous
- Streak
- White
- Density
- 2.75
- Cleavage
- On {001} perfect; on {110} indistinct.
- Fracture
- Brak danych
- Transparency
- Transparent,Translucent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Glauberite can be identified by its characteristic tabular or prismatic habit, vitreous luster, and relatively low hardness. Perfect cleavage in one direction is also a diagnostic feature. Its water solubility is an important distinguishing feature from many other minerals. ## Distinguishing from Similar Minerals Glauberite can be confused with other evaporite minerals such as gypsum or anhydrite. It is distinguished from gypsum by its greater hardness and lack of elasticity. It is distinguished from anhydrite by its lower hardness and the presence of sodium in its chemical composition. Water solubility is a key feature distinguishing it from many similar minerals. ## Crystal Forms Glauberite crystals most commonly occur in tabular, prismatic, or columnar forms. It often forms massive, granular, or fibrous aggregates. It can also occur as coatings or incrustations.
Geological environment
## Genesis Glauberite forms in evaporitic environments, i.e., as a result of the evaporation of saline waters, for example, in dry lake basins, lagoons, or marine sediments. It is a typical sedimentary mineral, forming under conditions of high salinity and arid climates. ## Mineral Associations It often co-occurs with other evaporite minerals such as halite, gypsum, anhydrite, polyhalite, thenardite, and other sulfates and chlorides. It can also be associated with clay minerals and carbonates. ## Localities Important glauberite deposits are found in Spain (e.g., in the Miranda de Ebro region), Austria (Hallstatt), Germany (Stassfurt), the United States (California, Arizona, New Mexico), and Russia (Volga region).
Rarity
Uncommon
For collectors
## Quality Criteria The most prized glauberite specimens are those with well-formed, transparent or translucent crystals with a distinct tabular or prismatic habit. The purity of the mineral, absence of mechanical damage, and an attractive aesthetic appearance are also important. Large, single crystals are more desirable than granular aggregates. ## Popular Localities Particularly prized specimens come from Spain, where large and well-formed crystals have been found. Other important localities include the United States, especially deposits in California, which provide interesting specimens for collectors.
Care and storage
## Cleaning Glauberite specimens should be cleaned gently, using a soft brush. Distilled water can be used to remove loose dirt, but prolonged soaking should be avoided as the mineral is water-soluble. ## What to Avoid Avoid contact with acids, which can damage the mineral. Due to its water solubility, storage in a humid environment is not recommended. Also avoid sudden temperature changes and exposure to direct sunlight, which can affect its color. ## Storage Glauberite is best stored in a dry place, away from sources of moisture and direct sunlight. Specimens should be protected from mechanical damage, for example, by placing them in soft material or in separate containers in a display cabinet.