Rewitzerite
Chemical formula: K(H₂O)Mn²⁺₂(Al₂Ti⁴⁺)(PO₄)₄[O(OH)](H₂O)₁₀·4H₂O
Rewitzerite is an extremely rare phosphate mineral, forming microscopic, yellow crystals, discovered in a quarry in Bavaria.
Properties
- Mohs hardness
- 2
- Color
- colorless
- Luster
- Vitreous
- Streak
- Light yellow
- Density
- 2.33
- Cleavage
- Perfect on {100}
- Fracture
- Uneven
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of Rewitzerite is impossible without advanced laboratory equipment. It requires chemical analysis (EDS) and structural analysis (XRD) to confirm its composition and crystal structure. Visually, under high magnification, characteristic, tiny, yellow crystals with a bladed habit can be observed. ## Distinguishing from Similar Minerals At the type locality, Rewitzerite may be confused with other yellow secondary phosphates. Distinguishing it from minerals such as Cacoxenite or Leucophosphite requires specialized analytical studies. ## Crystal Forms Rewitzerite forms very small, elongated, bladed crystals, often gathered in small, radial or chaotic aggregates on the surface of the host rock.
Geological environment
## Genesis Rewitzerite is a secondary mineral that crystallizes in the late stage of hydrothermal processes in phosphate-rich granitic pegmatites. It forms as a result of the alteration of pre-existing phosphate minerals in oxidation zones. ## Mineral Associations At the type locality, Rewitzerite is associated with quartz, Strengite, Leucophosphite, Rockbridgeite, Jahnsite-(CaMnMn), and other rare phosphates. ## Localities The only confirmed locality of Rewitzerite in the world is its type locality - the Hagendorf-Süd quarry in Waidhaus, Upper Palatinate, Bavaria (Germany).
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of a Rewitzerite specimen is assessed based on the abundance and development of microscopic crystals on the rock matrix. The most desirable specimens are those with numerous, clearly visible under the microscope, sharply terminated crystals forming aesthetic clusters. Contrast with the host rock color also enhances visual value. ## Popular Localities The only source of specimens is the Hagendorf-Süd quarry in Germany. Material from this locality is extremely difficult to obtain and appears on the market very rarely, mainly circulating among specialized micromount collectors.
Care and storage
## Cleaning Specimens containing Rewitzerite, due to the microscopic size and delicacy of the crystals, should not be cleaned mechanically or chemically. Any attempts at cleaning risk irreversible damage to the mineral. They should be left undisturbed on the host rock. ## What to Avoid Avoid contact with any liquids, chemicals, as well as changes in temperature and humidity. The crystals are brittle and sensitive to shocks and touch. Do not expose the specimen to direct sunlight. ## Storage Specimens should be stored exclusively in specialized, sealed "micromount" boxes, protecting them from dust, moisture, and mechanical damage. It is best to store them under stable room conditions.