Karasugite

Chemical formula: SrCaAlF₇

Karasugite is a rare fluoride of strontium, calcium, and aluminum, forming colorless, transparent, tabular crystals.

## Characteristics Karasugite is a very rare mineral from the halide group, specifically a complex fluoride of strontium, calcium, and aluminum. It occurs as small, tabular or bladed crystals, typically not exceeding 1 mm in length. The crystals are colorless and fully transparent, giving them a vitreous appearance. Due to its rarity and small size, it is a mineral known primarily in scientific circles and among specialized collectors. ## Physical Properties This mineral is characterized by a vitreous luster. Its density is approximately 3.06 g/cm³, which is a moderate value. It exhibits parting or cleavage in one plane, and its fracture is splintery. It is a relatively soft mineral. ## Colors and Varieties Karasugite is colorless. No colored varieties or trade names are known. ## History and Name The mineral's name comes from its discovery locality – the Karasug deposit in the Tuva Republic, Russia. It was first described and approved as a new mineral species in 1994. ## Uses Karasugite has no industrial applications. Its significance is purely scientific and collectible.

Properties

Luster
Vitreous
Streak
white
Density
3.06
Cleavage
Cleavage or parting {100}
Fracture
Splintery
Transparency
Transparent
Crystal system
Monoclinic

Diagnostic features

## Identification Amateur identification of karasugite is practically impossible due to its rarity and small crystal size. Identification requires advanced analytical methods, such as chemical composition analysis (EDS/WDS) and X-ray diffraction (XRD). It is distinguished by colorless, tabular crystals with a vitreous luster. ## Distinguishing from Similar Minerals It can be confused with other colorless minerals found in the same environment, such as fluorite, quartz, or calcite. Differentiation requires specialized studies, as physical characteristics (hardness, luster) are not sufficiently distinctive for unambiguous identification. ## Crystal Forms Karasugite forms small, tabular or bladed crystals, often gathered in small, radial aggregates.

Geological environment

## Genesis Karasugite is a hydrothermal mineral. It forms in the late stages of crystallization in carbonatite veins, rich in rare earth elements, strontium, barium, and fluorine. ## Mineral Associations This mineral co-occurs with other rare minerals such as bastnäsite, celestine, baryte, strontianite, as well as fluorite and calcite. ## Localities The only confirmed and described occurrence of karasugite in the world is its type locality – the Karasug deposit in the Tuva Republic, Russia.

Rarity

Very rare

For collectors

## Quality Criteria The quality of a karasugite specimen primarily depends on the presence of well-formed, sharp, and undamaged crystals, even if they are microscopic in size. Specimens where crystals are clearly visible on the rock matrix and form aesthetic groups are highly valued. Transparency and lack of inclusions also increase the specimen's value. ## Popular Localities The only source of karasugite specimens is the Karasug deposit in Russia, which makes every specimen from this locality valuable by definition.

Care and storage

## Cleaning Karasugite specimens should be cleaned with the utmost care, using only compressed air to remove dust. Due to the small size and delicacy of the crystals, contact with water and any mechanical tools, such as brushes, should be avoided. ## What to Avoid Contact with chemicals, especially acids, which can damage the mineral, should be avoided. It should also be protected from high temperatures and sudden temperature changes. Avoid ultrasonic cleaners. ## Storage Karasugite specimens, due to their small size and fragility, are best stored in specialized mineralogical boxes (micromount type) that protect them from mechanical damage, dust, and moisture.

External references

Sources

Read more