Ingersonite
Chemical formula: Ca<sub>3</sub>Mn<sup>2+</sup>Sb<sup>5+</sup><sub>4</sub>O<sub>14</sub>
Ingersonite is a very rare mineral from the oxide group, forming small, yellow-orange crystals with a regular crystallographic system.
Properties
- Mohs hardness
- 6
- Luster
- Adamantine
- Streak
- Pale yellow
- Density
- 5.55
- Cleavage
- None
- Fracture
- Conchoidal
- Transparency
- Transparent
- Crystal system
- Cubic
Diagnostic features
## Identification Identifying ingersonite under amateur conditions is practically impossible. Identification requires advanced analytical methods, such as chemical analysis (EDS/WDS) and X-ray diffraction (XRD). In a collection, it can be identified based on the label and provenance documentation. Visually, under high magnification, characteristic features include small, yellow-orange, octahedral crystals with an adamantine luster, occurring in the typical mineral association from Långban. ## Distinguishing from Similar Minerals Ingersonite may be confused with other rare, yellow minerals from the pyrochlore group or other antimony oxides. Certain differentiation is possible only based on chemical composition analysis, which is unique to this mineral. ## Crystal Forms Ingersonite crystallizes in the form of pyramidal, octahedral crystals (octahedra), usually not exceeding 0.3 mm in size. Crystals are most often single and grown on the surface of other minerals.
Geological environment
## Genesis Ingersonite forms in metamorphic manganese and iron skarn deposits. It is a product of hydrothermal or metamorphic processes occurring within these specific geological formations. It occurs in vugs and small rock fissures. ## Mineral Associations This mineral co-occurs with other, often rare, minerals characteristic of the Långban deposit. It is most commonly associated with calcite, hausmannite, magnussonite, katoptrite, berzeliite, and tegengrenite. ## Localities The only confirmed occurrence of ingersonite in the world is its type locality: the Långban mine, Filipstad municipality, Värmland region in Sweden. This is a classic mineralogical locality, known for the occurrence of many unique minerals.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of an ingersonite specimen is primarily determined by the size and quality of crystal formation, even though they are microscopic. Specimens with clearly visible, sharp, undamaged crystals of intense, yellow-orange color are most valued. The aesthetics of the rock matrix and the presence of rare associated minerals are also important. ## Popular Localities All known and valued ingersonite specimens come from a single location in the world – the historic Långban mine in Sweden. Specimens from this locality are classics and represent the only source of this mineral for collectors.
Care and storage
## Cleaning Ingersonite specimens, due to their extreme rarity and small crystal size, should be cleaned with the utmost care. It is recommended to only gently remove dust with a soft brush or a photographic air blower. Any contact with water or chemical agents should be avoided. ## What to Avoid Ultrasonic cleaners, all acids, detergents, and solvents must be absolutely avoided. The crystals are brittle, so the specimen should be protected from impacts, scratches, and vibrations. It should not be heated or exposed to sudden temperature changes. ## Storage Ingersonite specimens are best stored under stable conditions, in a sealed "micromount" box, which protects against dust and mechanical damage. Exposure to direct sunlight should be avoided, although there is no evidence of it fading.