SKUTTERUDITE – Rare Cobalt Arsenide, Silver Crystal Cluster, Bou Azzer, Morocco

Regular price €299,00
Sale price €299,00 Regular price
+ VAT
Unit price

A striking cluster of large, well-formed Skutterudite crystals displaying a brilliant tin-white to silver metallic luster. This cobalt-arsenic mineral rarely develops crystals of this size, making sizeable clusters like this one genuinely sought after by mineral collectors.

Mineral Data:

  • Dimensions: 118 x 91 x 51 mm
  • Weight: 711 g
  • Provenance: Bou Azzer mining district, Drâa-Tafilalet Region, Morocco
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SKUTTERUDITE – Rare Cobalt Arsenide, Silver Crystal Cluster, Bou Azzer, Morocco

SKUTTERUDITE – Rare Cobalt Arsenide, Silver Crystal Cluster, Bou Azzer, Morocco

Regular price €299,00
Sale price €299,00 Regular price
+ VAT
Unit price

This is an exceptional cluster of Skutterudite, a cobalt arsenide mineral that rarely forms crystals of appreciable size — most specimens on the market are massive or granular, which makes a cluster of this scale a genuine standout for serious collectors. The crystals display the classic tin-white to silver-gray metallic luster of the species, with faces showing the isometric habit typical of Skutterudite: cubes and octahedra, sometimes combined into more complex modified forms, catching the light with a bright, almost polished-looking sheen across the cluster.

The specimen comes from the Bou Azzer mining district in the Drâa-Tafilalet Region of Morocco, the world-famous cobalt-silver mining area of the Anti-Atlas Mountains and the source of the finest Skutterudite specimens available to collectors worldwide. Bou Azzer remains an active mining district today, one of the highest-grade cobalt deposits on the planet, and continues to yield the cobalt-nickel-iron arsenide minerals for which it is celebrated. The combination of size, metallic brilliance, and this classic Moroccan provenance make this cluster a fine addition to any systematic or aesthetic mineral collection.

Skutterudite is a cobalt arsenide mineral with the idealized formula CoAs3, in which nickel and iron commonly substitute for part of the cobalt, forming a continuous chemical series with nickel-rich and iron-rich varieties. Its bright, tin-white to silver-gray metallic color and lustrous surface come directly from its arsenide bonding structure rather than from any trace chromophore element: like many opaque metallic minerals, its electronic structure reflects most visible light almost uniformly, producing the characteristic bright metallic sheen. Over time, exposed surfaces can tarnish to a duller gray or develop faint iridescence as a thin oxidation layer forms.

Crystals typically develop in the isometric system, most often as cubes, octahedra, or more rarely dodecahedra, sometimes combined into modified or skeletal growth forms; well-formed crystal clusters of significant size, as in this specimen, are considered uncommon since Skutterudite more frequently occurs as massive or granular material. The mineral forms in moderate-to-high-temperature hydrothermal veins associated with serpentinized ophiolite complexes, alongside other cobalt and nickel arsenides such as safflorite and cobaltite — exactly the geological setting found at Bou Azzer, still an active mining district and one of the highest-grade cobalt deposits in the world.

  • Formula: CoAs3
  • Key chemical elements: Cobalt, Arsenic (with Nickel and Iron as common substitutions)
  • Hardness (Mohs scale): 5.5–6
  • Mineral class: Arsenides
  • Crystal system: Cubic (Isometric)
  • Crystal habit: Cubic, octahedral, occasionally dodecahedral; skeletal or distorted aggregates; massive/granular in most occurrences
  • Formation: Hydrothermal cobalt-nickel-iron arsenide veins associated with serpentinized Precambrian ophiolite
  • Color: Tin-white to silver-gray, metallic, tarnishing to dull gray or faint iridescence over time
  • Locality status: Active mining district

Skutterudite takes its name from Skuterud, a small mining area in Modum, Norway, where the mineral was first described in the 19th century. The Bou Azzer district in Morocco, however, is where the story of modern cobalt mining truly began: in 1928, a geologist strolling through Marrakech's famous Jemaa el-Fna square noticed a vividly colored cobalt mineral called erythrite on display, a discovery that eventually led prospectors to the Bou Azzer deposits.

Because Skutterudite contains arsenic, freshly broken or heated specimens can release a faint garlic-like odor — a classic field test long used by miners and geologists to help identify arsenic-bearing minerals. Despite decades of continuous extraction, Bou Azzer remains active today and is still regarded as one of the richest cobalt deposits ever discovered.

In crystal healing traditions, Skutterudite is associated with grounding energy and inner strength, thanks to its dense metallic structure and cool silver tones. Some practitioners of crystal therapy consider it a stone that helps clear mental fog and encourages focus and resilience during periods of change. Its shimmering, reflective surface is also said by some to symbolize clarity of thought and protection against negative energy.

As with all metaphysical attributions, these interpretations are not scientifically proven.

Photos: All photographs are taken under professional lighting conditions to accurately highlight crystal structure, color and detail. However, slight variations in tone and appearance may occur depending on screen calibration and ambient lighting conditions.

Shipping: is handled through selected reliable express couriers, with fast delivery (often 1–2 business days within Europe), full tracking, insurance coverage and professional protective packaging, as confirmed by customer feedback and reviews.

Multiple purchases can be consolidated into a single shipment, including items from different auctions or separate orders, by simply contacting us to arrange combined shipping. For high-value specimens, direct delivery by appointment is also available, either at home or at major European mineral shows and fairs.

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