Calcioancylite-(Nd)

Chemical formula: Nd₂.₈Ca₁.₂(CO₃)₄(OH)₃·H₂O

Calcioancylite-(Nd) is a rare mineral from the carbonate group, distinguished by its high neodymium content and occurrence as small, pinkish crystals.

## Characteristics Calcioancylite-(Nd) is a hydrated calcium and neodymium carbonate, belonging to the ancylite group. It forms very small, prismatic or dipyramidal crystals, rarely exceeding 1 mm in length. It typically occurs as single, well-formed crystals or small aggregates grown on other minerals. It is a transparent to translucent mineral with a vitreous luster. ## Physical Properties The mineral is characterized by a hardness of 4-4.5 on the Mohs scale and a density of approximately 4.34 g/cm³. It exhibits good cleavage in two directions and an uneven fracture. It is brittle. ## Colors and Varieties The typical color of calcioancylite-(Nd) is pale pink to pinkish, often with a violet hue. Colorless specimens are rarer. No commercial or colored varieties are distinguished. ## History and Name The mineral's name refers to its chemical composition – the dominance of calcium (Latin: *calcius*) and neodymium (Nd) – and its structural relationship to ancylite. It was first described in 1995 by P. Orlandi, M. Pasero, and A. Perchiazzi based on material from the Baveno quarry in Italy.

Properties

Mohs hardness
4-4.5
Color
Pale pink
Luster
Vitreous
Streak
White
Density
4.02
Cleavage
Good on {110}
Fracture
Irregular/Uneven
Transparency
Transparent
Crystal system
Monoclinic

Diagnostic features

## Identification Amateur identification of calcioancylite-(Nd) is practically impossible due to its small size and resemblance to other minerals of the ancylite group. Definitive identification requires advanced analytical methods, such as EDS spectroscopy or electron microprobe (EMPA), to confirm the chemical composition with dominant neodymium and calcium. ## Distinguishing from Similar Minerals It can be confused with other minerals from the same group, such as ancylite-(Ce), ancylite-(La), or calcioancylite-(Ce). They differ in the dominant rare earth element, which is impossible to determine without specialized analysis. Visually, it may also resemble other small, pink secondary minerals. ## Crystal Forms Crystals are most often prismatic, elongated, terminated by rhombohedral or dipyramidal faces. They occur as single, grown crystals or in small, loose groups.

Geological environment

## Genesis It is a hydrothermal mineral, crystallizing in the late stage from solutions rich in rare earth elements and carbonates. It forms in vugs and fissures in granites and syenites, often in Alpine-type pegmatites. ## Mineral Associations It most commonly co-occurs with quartz, orthoclase, albite, mica, as well as other rare minerals such as ewaldite, synchysite, bastnäsite, cordylite, burbankite, or fluorite. ## Localities The most important and classic localities for this mineral are the granite quarry in Baveno, Piedmont, Italy (type locality), and the Khibiny Massif on the Kola Peninsula in Russia. It has also been reported in Norway and Canada (Mont Saint-Hilaire).

Rarity

Very rare

For collectors

## Quality Criteria Most valued by collectors (mainly those specializing in "micromounts") are specimens with well-formed, sharp crystals of intense, pink coloration. Contrast with the matrix mineral on which the crystals are embedded, and the presence of associated minerals, are important. The size of the crystals, even if exceeding 1 mm, significantly increases the value of the specimen.

Care and storage

## Cleaning Specimens should only be cleaned very carefully, using a soft brush to remove dust. Due to the small size of the crystals and their brittleness, wet or mechanical cleaning is not recommended. ## What to Avoid Contact with acids, which cause vigorous effervescence and decomposition of the mineral, must be absolutely avoided. Avoid ultrasonics, steam cleaners, and strong detergents. The mineral is brittle, so it should be protected from impacts and scratching. ## Storage It is recommended to store specimens in sealed "micromount" boxes, which protect them from dust, mechanical damage, and sudden changes in humidity.

External references

Sources

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