ARAGONITE – Orange Star-Shaped Twin Cluster, Tazouta, Morocco

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A striking Aragonite specimen from the classic Tazouta locality in Morocco, showing a naturally sculptural star-shaped cluster of pseudohexagonal prismatic crystals. The warm brown-orange crystals are cyclically twinned, radiating outward from common centers in a globular, sputnik-like arrangement with glossy, well-defined faces. A fully natural, untreated piece of strong mineralogical and display value.

Mineral Data:

  • Dimensions: 58 x 48 x 46 mm
  • Weight: 123 g
  • Provenance: Tazouta diggings, Sefrou Cercle, Fès-Meknès Region, Morocco
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Close-up of pseudohexagonal aragonite twin crystals from Tazouta, Morocco

ARAGONITE – Orange Star-Shaped Twin Cluster, Tazouta, Morocco

Regular price €15,00
Sale price €15,00 Regular price
+ VAT
Unit price

This is a fully natural, untreated specimen of Aragonite from the famous Tazouta locality, Sefrou Cercle, Fès-Meknès Region, Morocco — one of the most iconic sources worldwide for aragonite crystal groups. The piece displays the classic pseudohexagonal prismatic crystals typical of this deposit, arranged in a distinctive globular, star-shaped cluster that collectors often nickname a 'sputnik' formation for its resemblance to a satellite bristling with antennae.

Each apparent hexagonal prism is in fact a cyclic twin, formed by three individual orthorhombic crystals intergrown on their prism faces, radiating outward from shared growth centers to produce the pseudo six-sided symmetry and the radial, star-like habit seen here. The crystal faces are glossy and crisply defined, with the aggregate built up in a compact globular mass rather than growing on a rock matrix.

The warm brown-orange coloration is characteristic of Tazouta aragonite, and the crystals show good luster across their terminated faces, enhancing the three-dimensional, radiating structure of the cluster.

Tazouta itself, near Sefrou in Morocco's Middle Atlas region, is often loosely referred to as a mine, though the aragonite groups are actually recovered from a natural open outcrop in reddish clay rather than from underground mining operations — a detail that adds to the geological character of material from this locality.

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