Okayamalite

Chemical formula: Ca₂B₂SiO₇

Okayamalite is a rare calcium borosilicate mineral, characterized by its creamy-white color and tetragonal crystallographic system.

## Characteristics Okayamalite is a calcium borosilicate mineral that typically occurs as fine-grained aggregates or as a component of rock masses. Its color is usually creamy-white, which is one of its characteristic visual features. Due to its rarity and mode of occurrence, well-formed okayamalite crystals are extremely rare. ## Physical Properties The Mohs hardness of okayamalite is 5.5. This mineral exhibits an earthy luster, giving it a dull appearance. It is transparent to translucent, meaning light can pass through it, but objects behind it are not clearly visible. The streak of okayamalite is white. ## Colors and Varieties Okayamalite primarily occurs in creamy-white shades. No significant color varieties or commercial names for this mineral are known. ## History and Name Okayamalite was named after Okayama Prefecture in Japan, where the mineral was first discovered. This name reflects its type locality. ## Uses Due to its rarity and lack of specific physical properties, okayamalite currently has no industrial applications. It is a mineral of scientific and collector's interest only.

Properties

Mohs hardness: 5.5
Luster: Earthy
Streak: white
Density: 0
Cleavage: Brak
Fracture: Nierówny
Transparency: Translucent
Crystal system: Tetragonal

Diagnostic features

## Identification Okayamalite can be identified by its creamy-white color, earthy luster, and a Mohs hardness of 5.5. Its occurrence as fine-grained aggregates in specific geological environments is also a diagnostic feature. ## Distinguishing from Similar Minerals Okayamalite can be confused with other white or creamy minerals with similar luster. Key distinguishing features are its hardness, streak, and precise chemical and diffraction analyses, which will confirm its unique borosilicate composition. ## Crystal Forms Okayamalite typically forms fine-grained aggregates. Well-formed crystals are very rare, but if they occur, they have a tetragonal habit.

Geological environment

## Genesis Okayamalite forms under specific metamorphic conditions, typically in boron skarns. These skarns form as a result of metasomatic alteration of carbonate rocks (e.g., limestones, dolomites) in contact with magmatic intrusions that supply boron and silicon. ## Mineral Associations Okayamalite often co-occurs with other skarn minerals, such as calcite, garnets (e.g., grossular), wollastonite, diopside, and other boron minerals. ## Localities The most important and type locality for okayamalite is the Fuka mine in Okayama Prefecture, Japan. This is also its discovery site.

Rarity

Extremely Rare

For collectors

## Quality Criteria The most prized okayamalite specimens are those that exhibit a distinct creamy-white color and, if possible, well-formed crystal habits, although these are extremely rare. Aggregates with a pure color and without visible impurities are also sought after. The size of the specimen is less important than its purity and aesthetic appeal. ## Popular Localities The most sought-after specimens come from the type locality, the Fuka mine in Okayama Prefecture, Japan.

Care and storage

## Cleaning Okayamalite can be cleaned gently using a soft brush and lukewarm water. For more stubborn dirt, distilled water can be used to avoid mineral deposits. ## What to Avoid Avoid using strong chemical agents, acids, and bases, which can damage the mineral's surface. Exposure to extreme temperature changes and direct, intense sunlight is also not recommended, as it can lead to changes in the specimen's appearance. The mineral should also be protected from excessive humidity. ## Storage Okayamalite should be stored in a dry place, away from direct sunlight and heat sources. It is best to place it in a closed container or display case to protect it from dust and mechanical damage. When storing with other minerals, ensure that delicate specimens will not be scratched or damaged.

External references

https://www.mindat.org/min-7202.html