Niahite
Chemical formula: (N<sup>3-</sup>H<sub>4</sub>)Mn<sup>2+</sup>PO<sub>4</sub>·H<sub>2</sub>O
Niahite is an extremely rare phosphate mineral, forming tiny, pale yellow crystals in caves as a product of guano reacting with manganese.
Properties
- Mohs hardness
- 1.5
- Luster
- Vitreous
- Streak
- White
- Density
- 2.45
- Cleavage
- Perfect on {010}
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Characteristic features of niahite include its occurrence environment (caves with guano deposits), extreme softness (Mohs hardness 1.5), pale yellow color, and water solubility. Its occurrence as tiny, tabular crystals in radiating aggregates is also a good indicator. ## Distinguishing from Similar Minerals Niahite can be confused with other rare cave phosphates such as struvite or newberyite. Struvite does not contain manganese and crystallizes in a different system. Newberyite also has a similar appearance and genesis. Reliable differentiation of these minerals under amateur conditions is practically impossible and usually requires advanced analyses, such as X-ray diffraction (XRD). ## Crystal Forms Niahite crystals are thin, flattened, tabular or bladed. They typically form fan-like or radiating aggregates and rosettes. They also occur as fine, dusty or earthy coatings on the host rock.
Geological environment
## Genesis Niahite is a secondary mineral, formed in the specific environment of karst caves. Its genesis is linked to the interaction of phosphate-rich solutions, derived from the decomposition of bat guano, with rocks or other manganese-containing minerals. ## Mineral Associations This mineral co-occurs with other phosphates typical of cave environments and guano deposits. It is most commonly associated with struvite, newberyite, hannayite, apatite, and brushite. ## Localities Niahite is an extremely rare mineral. Its main and essentially only well-documented occurrence is its type locality – the Great Cave of Niah in Sarawak, Borneo, Malaysia.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of niahite specimens is primarily assessed from a micromount collecting perspective. Samples with well-formed, sharp crystals forming aesthetic, radiating aggregates are most desirable. Rich mineralization on a small rock matrix and co-occurrence with other rare cave minerals are also highly valued. The clarity and transparency of the crystals, although difficult to assess with the naked eye, also increase the specimen's value. ## Popular Localities The only source of collectible specimens is the historical locality in the Great Cave of Niah in Malaysia. Finding this mineral on the market is an exceptional event.
Care and storage
## Cleaning Niahite is water-soluble, so **it must never be cleaned wet**. The only safe method is to very gently remove dust with a soft, dry brush (e.g., sable) or carefully use a stream of compressed air from a safe distance. ## What to Avoid Contact with water, water vapor, and all liquid chemicals must be strictly avoided. The mineral is very sensitive to moisture, which can damage or completely dissolve it. It is also very soft and brittle, so it must be protected from any impact, scratching, or vibrations. ## Storage Niahite specimens must be stored in completely dry conditions. It is recommended to keep them in tightly sealed containers (e.g., perky boxes) along with a desiccant (e.g., silica gel). They should be protected from dust and sudden temperature changes.