Pseudopomite

Chemical formula: Ca₃.₅[V₄+₆V₅+₉O₃₇(CO₃)]·₃₂H₂O

An extremely rare, hydrated calcium vanadate-carbonate, forming aggregates of black, tabular crystals.

## Characteristics Pseudopomaite is a complex, hydrated mineral from the vanadate group, also containing carbonate ions. It forms characteristic aggregates composed of very small, thin, tabular or platy crystals of black color and submetallic luster. It usually occurs as coatings and clusters on the surface of the host rock, which is sandstone. ## Physical Properties This mineral is very soft, with a Mohs hardness of approximately 2. It exhibits perfect, unidirectional cleavage, which, combined with its platy crystal habit, gives it a micaceous (scaly) fracture. It is opaque, and its density is about 2.45 g/cm³. The luster is described as submetallic. ## Colors and Varieties Pseudopomaite is a mineral of uniform, black color. No color varieties or commercial varieties are known. ## History and Name The mineral's name refers to its discovery locality – the Poma district in Salta Province, Argentina. It was described as a new mineral species in the 21st century, making it a relatively recently discovered mineral. ## Applications Due to its extreme rarity and occurrence in small quantities, pseudopomaite has no industrial applications. It is solely an object of scientific interest and a valuable acquisition for specialized collectors of rare minerals.

Properties

Mohs hardness: 2
Luster: Submetallic
Streak: Dark brown
Density: 2.45
Cleavage: Perfect on {001}
Fracture: Micaceous
Transparency: Opaque
Crystal system: Tetragonal

Diagnostic features

## Identification Characteristic features of pseudopomaite include its black color, submetallic luster, occurrence as coatings or aggregates of small, platy crystals, and very low hardness. A key diagnostic clue is its unique occurrence locality. ## Distinguishing from Similar Minerals Pseudopomaite can be confused with other black secondary minerals with a platy habit, such as some micas (e.g., biotite) or other rare vanadates. Final and certain distinction from similar minerals requires advanced analytical methods, such as X-ray diffraction (XRD) or chemical microanalysis (EDS). ## Crystal Forms Pseudopomaite crystals are very small, thin, and tabular, with a square or rectangular outline. They usually form dense, rosette-like or platy aggregates and coatings on the surface of the host rock.

Geological environment

## Genesis Pseudopomaite is a secondary mineral. It forms in the weathering zone of vanadium deposits, under desert or semi-desert climatic conditions. It forms as a product of the alteration of earlier vanadium minerals, crystallizing as coatings (efflorescences) on the surface of permeable rocks, such as sandstones. ## Mineral Associations It occurs directly on a sandstone matrix. It co-occurs with other secondary vanadium minerals typical of this type of geological environment. ## Localities The only confirmed occurrence of pseudopomaite in the world is its type locality in the Poma district, Salta Province, northwestern Argentina.

Rarity

Extremely rare

For collectors

## Quality Criteria The quality of specimens of this rare mineral is primarily assessed based on the richness and abundance of aggregates on the host rock. Samples with dense, well-formed crystalline clusters that clearly stand out from the substrate are most valued. The absence of mechanical damage to the delicate crystals is also important. ## Popular Localities The only collectible specimens come from the mineral's discovery locality in the Poma district, Argentina. It is an extremely difficult mineral to acquire, found almost exclusively in institutional collections and among highly specialized collectors of rare species.

Care and storage

## Cleaning Pseudopomaite specimens are extremely delicate and sensitive. Cleaning should be limited to very carefully removing dust with a soft brush or a stream of compressed air from a safe distance. Absolutely avoid contact with water and any chemical agents. ## What to Avoid The mineral is very sensitive to dehydration. Avoid exposure to heat, direct sunlight, and dry air, which can lead to its disintegration. It is very soft and brittle, so it must be protected from any impact or abrasion. Contact with water can cause damage. ## Storage It is recommended to store specimens in closed, stable conditions, preferably in "micromount" boxes, which protect against mechanical damage, dust, and humidity fluctuations. Keep it away from sources of heat and light.

Sources

IMA Mineral List (CNMNC)