Niningerite

Chemical formula: MgS<sup>2-</sup>

Niningerite is a rare magnesium sulfide, found almost exclusively in meteorites known as enstatite chondrites.

## Characteristics Niningerite is a sulfide mineral belonging to the galena group. It occurs as very small, individual grains or aggregates, usually submillimeter in size, dispersed within the meteorite's rock mass. Its crystals, when visible, adopt cubic or octahedral forms. Due to its origin and small size, it is primarily of scientific interest rather than a typical collector's item. ## Physical Properties Niningerite is characterized by a hardness ranging from 3.5-4 on the Mohs scale. It has a metallic luster and is opaque. Its density is approximately 2.91 g/cm³. It exhibits perfect cubic cleavage in three directions. ## Colors and Varieties This mineral is gray to black in color. It does not form color varieties or commercial varieties. ## History and Name Niningerite was first described in 1967 based on material from the Abee meteorite, which fell in Canada. The mineral is named in honor of Harvey Harlow Nininger (1887-1986), an American pioneer in meteorite research, who made immense contributions to their collection and the popularization of meteoritics. ## Uses Niningerite has no industrial applications. Its significance is purely scientific, providing information about the conditions in the early Solar System where the parent bodies of enstatite chondrites formed.

Properties

Mohs hardness
3.5-4
Luster
Metallic
Streak
Black
Density
2.91
Cleavage
Perfect on {100}
Fracture
Uneven
Transparency
Opaque
Crystal system
Cubic

Diagnostic features

## Identification Identifying niningerite is extremely difficult without specialized equipment. It requires chemical analysis (e.g., using an electron microprobe) and X-ray diffraction (XRD) to confirm its composition (magnesium sulfide) and crystal structure. Visually, it is simply a small, black or gray, metallic grain within the meteorite rock. ## Distinguishing from Similar Minerals It can be confused with other fine-grained, opaque minerals found in meteorites, such as troilite (FeS), graphite (C), or chromite. Differentiation relies solely on laboratory analysis of chemical composition – niningerite is distinguished by its high magnesium content. ## Crystal Forms It forms very small, isometric crystals with a cubic or octahedral habit. Most often, it occurs as irregular grains intergrown with other minerals.

Geological environment

## Genesis Niningerite is a mineral characteristic of a very specific environment – enstatite chondrites. These are meteorites that formed under highly reducing (anaerobic) conditions and at high temperatures, likely in the inner part of the solar nebula. Under such conditions, magnesium, instead of forming silicates, combined with sulfur. ## Mineral Associations This mineral co-occurs with other minerals typical of enstatite chondrites, such as enstatite, clinoenstatite, kamacite, perryite, oldhamite, troilite, and various phosphides and silicides of metals. ## Localities Its occurrence is limited to enstatite chondrites. It has been identified, among others, in the Abee meteorite (Alberta, Canada – type locality), Adhi Kot (Pakistan), Indarch (Azerbaijan), Qingzhen (China), and Saint-Sauveur (France).

Rarity

Very rare

For collectors

## Quality Criteria From a collector's perspective, the value of a specimen containing niningerite primarily depends on the value of the meteorite itself in which it is found. Since niningerite grains are microscopic, their individual quality is not assessed. What matters is the well-documented provenance of the meteorite and the presence of the mineral confirmed by analyses. The most valuable specimens are those from type localities or from rare, well-studied falls. ## Popular Localities The most known and historically important source is the Abee meteorite from Canada. Other meteorites in which niningerite has been identified, such as Indarch or Qingzhen, are also valued by collectors specializing in meteorites.

Care and storage

## Cleaning Specimens containing niningerite, due to their sensitivity to moisture and oxygen, should generally not be wet-cleaned. Dust can be removed very carefully with a soft brush or compressed air from a safe distance. ## What to Avoid Contact with water, water vapor, and high humidity must be strictly avoided, as niningerite readily reacts with water, undergoing decomposition. It must also be protected from oxygen, which causes its oxidation. No chemical agents should be used. ## Storage Storage requires specialized conditions. Specimens are best kept in airtight containers with a desiccant (silica gel) or in an inert gas atmosphere (e.g., argon). Display should be in closed, sealed showcases with controlled humidity.

External references

Sources

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