Waterhouseite
Chemical formula: Mn²⁺₇(PO₄)₂(OH)₈
Waterhouseite is a rare, hydrated manganese phosphate, forming orange-brown, tabular crystals with a vitreous luster.
Properties
- Mohs hardness
- 4
- Luster
- Vitreous
- Streak
- Yellowish brown
- Density
- 3.55
- Cleavage
- on (100), indistinct on (001)
- Fracture
- Conchoidal
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Waterhouseite can be identified by its characteristic orange-brown color, tabular crystal habit, often forming rosette-like aggregates, and vitreous luster. A yellowish-brown streak is also helpful in identification. Its occurrence in paragenesis with other manganese minerals in iron deposits is also an important clue. ## Distinguishing from Similar Minerals This mineral can be confused with other manganese phosphates of similar color, such as dickinsonite or fillowite. Distinguishing it often requires advanced research methods, such as X-ray diffraction (XRD), due to the similarity of physical properties. Key factors are a careful examination of crystal habit and mineral paragenesis. ## Crystal Forms Waterhouseite crystals are typically thin, tabular or bladed, flattened parallel to the (100) plane. They often occur as fan-shaped or rosette-like aggregates, where individual crystals radiate from a common center.
Geological environment
## Genesis Waterhouseite is a secondary mineral that forms in the oxidation zones of iron and manganese ore deposits. It originates from the alteration of primary phosphate minerals in a manganese-rich environment. ## Mineral Associations This mineral co-occurs with other secondary phosphate minerals and oxides. In its type locality (Iron Monarch in Australia), it was found in association with shigiite, gatehouseite, arsenoclasite, hematite, barite, and quartz. ## Localities The most important and also the type locality for waterhouseite is the Iron Monarch mine in the Iron Knob region of South Australia. This is currently the only confirmed locality where this mineral has been identified, making it extremely rare on a global scale.
Rarity
Very rare
For collectors
## Quality Criteria Specimens with well-formed, sharp crystals forming aesthetic, rosette-like or fan-shaped aggregates are most valued by collectors. The intensity and attractiveness of the orange-brown color and the transparency of the crystals are important. Specimens on a contrasting matrix, for example with hematite, are particularly desirable. Due to its rarity, any well-defined specimen is valuable. ## Popular Localities The only source of waterhouseite specimens is its type locality – the Iron Monarch mine in South Australia. All specimens available on the collector's market originate from this single location.
Care and storage
## Cleaning Waterhouseite specimens should be cleaned very carefully, using a soft brush to remove dust. If wet cleaning is necessary, distilled water is recommended, and prolonged soaking should be avoided. After cleaning, the specimen should be thoroughly dried. ## What to Avoid Contact with acids and other aggressive chemicals, which can damage the mineral, should be avoided. Due to its relatively low hardness, it is susceptible to scratches, so it must be protected from contact with harder minerals. Ultrasonic cleaners should also be avoided. ## Storage Waterhouseite specimens are best stored in separate, padded display boxes to prevent abrasion and mechanical damage. Protect from dust and moisture. It does not require special protection from light.