Magnesiohögbomite-2<i>N</i>4<i>S</i>
Chemical formula: (Mg<sub>8.43</sub>Fe<sup>2+</sup><sub>1.57</sub>)Al<sub>22</sub>Ti<sup>4+</sup><sub>2</sub>O<sub>46</sub>(OH)<sub>2</sub>
Magnesiohögbomite-2N4S is a very rare, black mineral from the högbomite group, found in magnesium-rich metamorphic rocks.
Properties
- Mohs hardness
- 7.5-8
- Luster
- Metallic
- Streak
- Black
- Density
- 3.81
- Cleavage
- None
- Fracture
- Uneven
- Transparency
- Opaque
- Crystal system
- Hexagonal
Diagnostic features
## Identification Identification of magnesiohögbomite-2N4S is extremely difficult and practically impossible without advanced analytical methods, such as X-ray microanalysis (EDS/WDS) and X-ray diffraction (XRD). In collections, it is identified based on the label and confirmed analysis from the provenance. Visually, it is simply a black, microscopic inclusion. ## Distinguishing from Similar Minerals It can be confused with other black minerals included in corundum, such as hercynite, magnetite, ilmenite, or other minerals from the högbomite group. Differentiation requires specialized laboratory equipment. ## Crystal Forms It forms small, hexagonal, tabular crystals, often with a prismatic habit. It usually occurs as single, isolated crystals embedded in the host mineral.
Geological environment
## Genesis It forms under conditions of high-grade metamorphism, in aluminum- and magnesium-rich rocks. In its type locality (Mautia Hill, Tanzania), it occurs in a rock called rodingite, which formed as a result of metasomatism associated with the serpentinization of ultramafic intrusions. ## Mineral Associations It co-occurs with minerals such as corundum (often as an inclusion), anorthite, clinochlore, dolomite, spinel, geikielite, and titanite. ## Localities The most important and type locality is Mautia Hill in the Kongwa region, Dodoma, Tanzania. This is the only confirmed and well-documented locality for this mineral worldwide.
Rarity
Extremely rare
For collectors
## Quality Criteria For collectors, the most important criterion is the confirmation of the specimen's authenticity through chemical analysis. The size and quality of the crystals are of secondary importance, as they are always microscopic. The most desirable specimens are those where the magnesiohögbomite crystal is clearly visible against a contrasting host mineral, such as light-colored corundum. ## Popular Localities The only source of collector specimens is the type locality in Tanzania (Mautia Hill).
Care and storage
## Cleaning Specimens, typically as inclusions in corundum, can be gently cleaned with compressed air to remove dust. Mechanical or chemical cleaning is not recommended due to the risk of damaging the microscopic crystals. ## What to Avoid Avoid contact with acids and strong chemicals. Despite its high hardness, specimens are brittle and should be protected from impacts and scratching. ## Storage Store in stable conditions, away from dust and moisture, preferably in a sealed "micromount" box. Exposure to strong light is not harmful, but also not necessary.