Lanthanite-(Ce)
Chemical formula: Ce³⁺₂(CO₃)₃(H₂O)₆·2H₂O
Lanthanite-(Ce) is a rare, hydrated cerium carbonate, forming small, tabular crystals with a pearly or vitreous luster, often in shades of pink and white.
Properties
- Mohs hardness
- 2.5
- Color
- Yellowish white, pink, colourless
- Luster
- Pearly, Vitreous, Earthy
- Streak
- White
- Density
- 2.76
- Cleavage
- {010}
- Fracture
- Uneven
- Transparency
- Transparent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Lanthanite-(Ce) can be identified by its characteristic, thin, tabular crystals, often forming rosette-like aggregates. Key features include very low hardness (2.5), perfect cleavage in one direction, and a pearly luster on cleavage planes. It often has a characteristic pinkish hue. It reacts vigorously with acids, releasing carbon dioxide. ## Distinguishing from Similar Minerals It can be confused with other minerals from the lanthanite group, such as lanthanite-(La) and lanthanite-(Nd). Differentiation between them is only possible using advanced analytical methods, such as EDS or WDS spectroscopy. From other carbonates (e.g., calcite), it is distinguished by its lower hardness, specific crystal form, and often pink color. ## Crystal Forms Crystals are typically thin-tabular, with a rhombic or pseudohexagonal outline. They usually occur as fan-shaped, rosette-like, or radiating aggregates. It is also found as earthy and powdery coatings and crusts.
Geological environment
## Genesis Lanthanite-(Ce) is a secondary mineral formed in the oxidation (weathering) zones of ore deposits and pegmatites rich in rare-earth elements. It forms as a result of the alteration and decomposition of primary cerium-bearing minerals, such as allanite, cerite, bastnäsite, or monazite. It is a product of processes occurring near the Earth's surface, under low temperature and pressure conditions. ## Mineral Associations It often co-occurs with the minerals from which it forms, such as allanite-(Ce), cerite-(Ce), bastnäsite-(Ce), as well as other secondary rare-earth minerals, calcite, fluorite, and various iron oxides. ## Localities Significant localities from which well-formed specimens originate include the Bastnäs mine in Riddarhyttan (Sweden) - the type locality. Other known localities include Curitiba in Parana state (Brazil), the Niobec mine in Quebec (Canada), and some localities in the USA (e.g., in Pennsylvania and New Mexico).
Rarity
Rare
For collectors
## Quality Criteria Most valued by collectors are specimens with well-formed, sharp crystals forming aesthetic, rosette-like or fan-shaped aggregates. The intensity of the pink color significantly enhances the attractiveness of the specimen. The size of the crystals is also important – although the mineral forms small shapes, specimens with crystals exceeding a few millimeters are rare. A contrasting matrix is also desirable. ## Popular Localities The historical Bastnäs locality in Sweden is considered classic and yields the best specimens. High-quality microcrystals also come from Curitiba, Brazil.
Care and storage
## Cleaning Lanthanite-(Ce) specimens are extremely delicate and sensitive. Mechanical cleaning is not recommended. If absolutely necessary, a stream of compressed air can be used to remove loose dust. Avoid contact with water, as the mineral is partially soluble and can be damaged. ## What to Avoid Absolutely avoid contact with water, acids, and other chemicals. The mineral is very soft, susceptible to scratches and mechanical damage. Protect it from high temperatures and direct sunlight, which can cause dehydration and structural changes. ## Storage It is recommended to store specimens in sealed, airtight boxes (e.g., "micromount" type), away from dust, humidity, and temperature fluctuations. Due to its fragility, it should not be stored in contact with harder minerals.