Suolunite
Chemical formula: Ca<sub>2</sub>Si<sub>2</sub>O<sub>5</sub>(OH)<sub>2</sub>·H<sub>2</sub>O
Suolunite is a rare hydrated calcium silicate, forming characteristic fibrous or acicular aggregates with a silky luster.
Properties
- Mohs hardness
- 4.5
- Luster
- Vitreous to Silky
- Streak
- White
- Density
- 2.56
- Cleavage
- Perfect on {010}
- Fracture
- Uneven
- Transparency
- Translucent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Characteristic features of suolunite include its fibrous or acicular habit, often in the form of radial aggregates, and its white color and silky luster. Its specific occurrence environment – rodingites within ultramafic rocks (serpentinites) – is also crucial for identification. ## Distinguishing from Similar Minerals Suolunite can be confused with other white, fibrous minerals, such as xonotlite, okenite, or some zeolites (e.g., natrolite). Xonotlite is harder and more compact. Okenite forms very delicate, fluffy aggregates resembling cotton. Natrolite has a similar habit but different optical properties and occurs in a different geological environment (cavities in volcanic rocks). Definitive differentiation often requires X-ray diffraction (XRD) analysis. ## Crystal Forms Suolunite forms very fine, elongated crystals with an acicular or hair-like habit. These crystals almost always occur as dense fibrous aggregates, as well as radial or spherulitic aggregates.
Geological environment
## Genesis Suolunite is a low-temperature hydrothermal mineral. It forms as a result of metasomatic processes, where calcium-rich solutions interact with ultramafic rocks, such as serpentinites. It is a typical component of rodingites – rocks formed by this process, often within ophiolite complexes. ## Mineral Associations This mineral often co-occurs with other calcium silicates and minerals typical of rodingites, such as diopside, vesuvianite, prehnite, xonotlite, hydrogrossular, and chlorite. ## Localities The most important and well-documented suolunite localities in the world are few. They include the type locality in the Suolun-Hegenshan ophiolite complex in China, Wurlali volcano on Damar Island in Indonesia, and occurrences within the Hatrurim Formation in Israel.
Rarity
Very rare
For collectors
## Quality Criteria The most prized specimens by collectors are those with well-formed, spherical or radial aggregates with a distinct silky luster. Samples where suolunite contrasts colorfully with the rock matrix or co-occurs with other well-formed minerals, such as vesuvianite or diopside, are also highly valued. Due to the small size of the crystals, the size of the aggregates is also an important factor. ## Popular Localities The most famous specimens, which serve as reference material for this species, come from the type locality in Inner Mongolia, China. Specimens from other localities, such as Indonesia or Israel, are also sought after due to their rarity.
Care and storage
## Cleaning Suolunite specimens should be cleaned very carefully, preferably with a soft brush dry to remove dust. If necessary, compressed air can be used. Contact with water, especially for extended periods, is not recommended. If absolutely necessary, use distilled water and immediately dry the specimen thoroughly. ## What to Avoid Avoid ultrasonic cleaners, chemical agents, and especially acids. The mineral is relatively soft and brittle, so it must be protected from impacts and scratching by harder minerals. As a hydrated mineral, it may be sensitive to high temperatures. ## Storage Collector's specimens of suolunite are best stored in separate, padded boxes to prevent mechanical damage. They should be protected from dust and moisture.