Lovdarite
Chemical formula: K<sub>2</sub>Na<sub>6</sub>Be<sub>4</sub>Si<sub>14</sub>O<sub>36</sub>·9H<sub>2</sub>O
Lowdarite is a rare beryllium, potassium, and sodium silicate, forming characteristic spherical aggregates of fine, prismatic crystals.
Properties
- Mohs hardness
- 5
- Luster
- Vitreous
- Streak
- White
- Density
- 2.33
- Cleavage
- Good on {100} and {010}
- Fracture
- Uneven
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Lowdarite is most easily recognized by its characteristic mode of occurrence – small, white or colorless spheres (spherulites) with a radial internal structure. These aggregates usually have a vitreous luster. It occurs in a specific geological environment – in nepheline-syenite pegmatites. ## Distinguishing from Similar Minerals It can be confused with other zeolites or minerals forming spherulitic aggregates, such as natrolite, thomsonite, or some forms of calcite. It is often distinguished from natrolite by its more spherical aggregate form (natrolite tends to form radial fans or needles). However, definitive differentiation requires advanced analytical methods, such as X-ray diffraction (XRD). ## Crystal Forms Crystals are prismatic or acicular, very small, usually not exceeding 1 mm. They almost always occur as radial or spherulitic aggregates up to several millimeters in diameter.
Geological environment
## Genesis Lowdarite is a hydrothermal mineral. It forms in the late stages of crystallization of highly alkaline pegmatites, crystallizing in vugs and fissures. It is a product of the alteration of other, previously formed minerals. ## Mineral Associations This mineral co-occurs with other rare minerals typical of alkaline massif pegmatites. It is most often associated with: eudialyte, nepheline, microcline, aegirine, lorenzenite, vuonnemite, zorite, and natrolite. ## Localities The most important and classic localities for lowdarite are found in the alkaline massifs of the Kola Peninsula in Russia, especially in the Lovozero Massif (e.g., Karnasurt, Kedykvyrpak, Alluaiw mountains) and in the Khibiny Massif. These are the main sources of the best-formed specimens in the world.
Rarity
Very rare
For collectors
## Quality Criteria The most prized lowdarite specimens are those with well-formed, distinct spherulites at least several millimeters in diameter, contrastingly set on a rock matrix. Specimens with visible, individual crystals forming the aggregate are desirable. Purity (lack of damage) and aesthetic composition with other rare associated minerals (e.g., eudialyte) significantly increase their collector's value. ## Popular Localities Specimens from the type locality – the Lovozero Massif on the Kola Peninsula in Russia – are by far the most sought after by collectors. Material from this region is considered exemplary for this species.
Care and storage
## Cleaning Lowdarite specimens should be cleaned very carefully, using a soft brush to remove dust. Due to its brittleness and solubility in acids, washing in water, especially in chemical solutions, should be avoided. If it is necessary to remove loose contaminants, compressed air can be used from a safe distance. ## What to Avoid Avoid contact with water and chemicals, particularly acids, in which lowdarite decomposes. The mineral is brittle, so it must be protected from impacts and vibrations. It should not be heated, as it contains water in its structure. ## Storage It is recommended to store specimens in closed, stable containers or display cases to protect them from dust, moisture, and mechanical damage. It is best to keep it away from other, harder minerals that could scratch it.