Nepouite
Chemical formula: Ni<sup>2+</sup><sub>3</sub>Si<sub>2</sub>O<sub>5</sub>(OH)<sub>4</sub>
Nepouite is a rare, green nickel mineral of the serpentine group, forming in hydrothermal environments.
Properties
- Mohs hardness
- 2-3
- Luster
- Woskowy do matowego
- Streak
- Jasnozielona do białej
- Density
- 2.6-2.8
- Cleavage
- Doskonała wg {001}
- Fracture
- Nierówny
- Transparency
- Przeświecający do nieprzezroczystego
- Crystal system
- Monoclinic
Diagnostic features
## Identification Nepouite can be identified by its characteristic green color, waxy or dull luster, and low hardness. It often occurs as compact masses or coatings. Its association with other nickel minerals, such as garnierite, can also indicate its presence. ## Distinguishing from Similar Minerals Nepouite is sometimes confused with other green nickel minerals, especially garnierite, which is a mixture of various hydrated nickel silicates. It is usually distinguished from garnierite by its more uniform color and chemical composition. It can also be confused with some serpentines, but its intense green color and the presence of nickel are diagnostic features. ## Crystal Forms Nepouite rarely forms well-developed crystals. It most commonly occurs as fine-grained, compact aggregates, coatings, incrustations, or platy masses. Crystals, if present, are usually acicular or platy and very small.
Geological environment
## Genesis Nepouite forms under low-temperature, hydrothermal conditions, often in weathering zones of ultramafic rocks rich in nickel. It is a product of alteration of serpentinites and peridotites, where nickel released from primary minerals (e.g., olivine) is incorporated into the silicate structure. ## Mineral Associations Nepouite often co-occurs with other nickel minerals, such as garnierite, chrysotile, lizardite, antigorite, as well as with quartz, chalcedony, and iron minerals. ## Localities The most important nepouite localities are in New Caledonia (Nepoui mine), where it was discovered. Other known occurrences include Greece (Lokris), United States (Oregon, California), Russia (Urals), and Australia.
Rarity
Rare
For collectors
## Quality Criteria The most prized nepouite specimens are those with an intense, uniform green color, free from visible impurities. Large, compact masses or specimens with well-formed, though small, crystals are more desirable. Color purity and the absence of cracks or mechanical damage also contribute to its collector's value. ## Popular Localities The most sought-after specimens come from New Caledonia, especially from the vicinity of the Nepoui mine, due to its historical significance and often high quality of finds there.
Care and storage
## Cleaning Nepouite is a relatively soft mineral, so it should be cleaned gently. It is best to use a soft cloth or brush to remove dust. For heavier soiling, lukewarm water with a small amount of mild soap can be used, followed by thorough rinsing and drying. Avoid vigorous scrubbing. ## What to Avoid Avoid contact of nepouite with strong acids and bases, which can damage its surface. Due to its softness, protect it from scratches. Prolonged exposure to direct sunlight can lead to color fading. Avoid sudden temperature changes. ## Storage Nepouite is best stored in enclosed display cases or boxes, away from dust and other minerals that could scratch it. An ideal location has stable temperature and humidity. Specimens can be displayed in shaded areas to preserve their natural color.