Harrisonite

Chemical formula: CaFe²⁺₆(SiO₄)₂(PO₄)₂

Harrisonite is a rare calcium iron silicophosphate, forming small, transparent, yellowish-brown crystals.

## Characteristics Harrisonite is a mineral from the silicophosphate group, characterized by the presence of calcium and iron in its structure. It occurs as small, spheroidal or hemispherical aggregates, which can reach up to 1 mm in diameter. Individual crystals within these aggregates are tabular or platy. Typical specimens are yellowish-brown to orange-brown and exhibit a vitreous luster. ## Physical Properties This mineral is transparent to translucent. Its Mohs hardness is 4-5, placing it in the category of medium-hard minerals. The density of harrisonite is approximately 4.02 g/cm³. It is characterized by a conchoidal fracture. ## Colors and Varieties Harrisonite occurs in shades of brown, from yellowish-brown to orange-brown. No color varieties or commercial varieties have been distinguished. ## History and Name The mineral was discovered in 1991 on Arcedeckne Island in the Kitikmeot region (Nunavut territory, Canada). Its name honors Robert "Bob" D. Harrison (born 1954), a Canadian electron microscopy technician from the University of Manitoba, who made significant contributions to mineral research in this region.

Properties

Mohs hardness
4-5
Luster
Vitreous
Streak
Pale yellow
Density
4.02
Fracture
Conchoidal
Transparency
Transparent,Translucent
Crystal system
Trigonal

Diagnostic features

## Identification Identification of harrisonite is based on its unique occurrence environment, characteristic form of spheroidal aggregates, yellowish-brown color, and relatively high density. The streak is pale yellow. Final confirmation requires advanced analytical methods, such as X-ray diffraction (XRD) or chemical analysis. ## Distinguishing from Similar Minerals It can be confused with other fine-grained phosphate or silicate minerals of similar color. It is distinguished by its co-occurrence with other rare minerals in a specific geological environment and its characteristic pale yellow streak. ## Crystal Forms Harrisonite forms spheroidal or hemispherical aggregates composed of small, tabular crystals. Individual crystals are too small to be observed without magnification.

Geological environment

## Genesis Harrisonite forms as a result of metamorphic processes under specific conditions. At its type locality (Arcedeckne Island), it occurs in metasomatically altered silicate xenoliths that were trapped within basaltic volcanic rock. ## Mineral Associations This mineral co-occurs with other rare minerals such as zoltaiite, brassiite, dmitryivanovite, iwakite, as well as hematite, ilmenite, graphite, and fayalite. ## Localities The only confirmed and described locality of harrisonite in the world is its type locality – Arcedeckne Island in the Kitikmeot region, Nunavut territory, Canada.

Rarity

Extremely rare

For collectors

## Quality Criteria As a "micromount" type mineral, its collector's value primarily depends on the quality and size of the spheroidal aggregates, their good development, and aesthetic placement on the host rock (matrix). The richness of its association with other rare minerals is also important. ## Popular Localities The only source of harrisonite specimens is its type locality on Arcedeckne Island in Canada, which makes every specimen from this locality extremely valuable to specialized collectors.

Care and storage

## Cleaning Due to the rarity and small size of the crystals, mechanical cleaning is not recommended. If absolutely necessary, compressed air can be used to remove dust. Avoid contact with water and chemicals. ## What to Avoid Avoid ultrasonic cleaners, strong chemicals, acids, and sudden temperature changes. The mineral is relatively soft, so it must be protected from scratching by harder minerals. ## Storage Harrisonite specimens, being extremely rare and small, should be stored in specialized "micromount" boxes that protect them from mechanical damage and dust. Avoid exposure to moisture.

External references

Sources

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