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  • Andradite Garnet Morocco Khenifra Tafilalet Mineral Specimen 40-60mm

Andradite Garnet Morocco Khenifra Tafilalet Mineral Specimen 40-60mm

$18.02 $34.6
Description Andradite Garnets – Khenifra Province, Tafilalet, Morocco (40–60mm) This Andradite Garnet specimen from Khenifra Province, Tafilalet, Morocco is a genuine natural mineral piece, carefully selected for its crystal form, colour, and collector appeal. Measuring approximately 40–60mm (full sizing please see photo), this is a carefully chosen specimen, and the photograph provided shows an example of the actual piece you will receive. Each item includes a Certificate of Authenticity lifetime guarantee generic card, confirming it as a genuine mineral specimen. Mineral Species & Chemical Composition Andradite is a calcium iron garnet with the chemical formula: Ca₃Fe₂(SiO₄)₃ It belongs to the garnet group of nesosilicate minerals, which crystallise in the isometric (cubic) crystal system. Like all garnets, andradite forms symmetrical crystals, often displaying classic geometric habits such as: Dodecahedral crystals Trapezohedral forms Complex intergrown crystal clusters Andradite has a hardness of approximately 6.5–7 on the Mohs scale, making it a durable and display-worthy mineral. Its vitreous to subadamantine lustre enhances the reflective quality of well-formed crystal faces. Colour, Lustre & Crystal Characteristics Andradite garnets from Morocco commonly display rich earthy tones, which may include: Brown to reddish-brown Yellow-brown or honey hues Dark olive or nearly black tones in some examples Crystal faces may show a bright reflective surface, and well-developed specimens often exhibit sharp edges and symmetrical growth patterns. Depending on lighting, the crystals may appear opaque to slightly translucent at thinner edges. Each 40–60mm specimen is unique in crystal arrangement and surface detail, with natural variations reflecting its geological history. Geological Formation & Moroccan Locality The Khenifra Province in the Tafilalet region of Morocco is internationally recognised for producing high-quality garnet specimens. These andradite garnets typically form in skarn deposits, which develop when igneous intrusions interact with carbonate-rich sedimentary rocks. In these environments, heat and mineral-rich fluids cause chemical reactions between magma and surrounding limestone or dolomite, leading to the formation of calcium-rich silicate minerals such as garnet. Associated minerals in Moroccan skarn deposits may include: Magnetite Calcite Pyroxene Epidote Quartz The geological complexity of the Tafilalet region contributes to the well-formed and aesthetically pleasing garnet crystals found there. Size, Presentation & Authenticity Mineral: Andradite Garnet Chemical Formula: Ca₃Fe₂(SiO₄)₃ Crystal System: Isometric (Cubic) Origin: Khenifra Province, Tafilalet, Morocco Size: Approximately 40–60mm (please refer to photo for full sizing reference) Authenticity: Includes Certificate of Authenticity lifetime guarantee generic card This specimen is ideal for mineral collectors, garnet enthusiasts, skarn mineral collectors, educational geology collections, or as a distinctive natural history display piece. The 40–60mm size provides strong cabinet presence and visual impact. Collecting & Traditional Associations Andradite garnet is highly valued among collectors for its well-formed crystals and association with classic skarn mineral environments. Moroccan specimens are particularly sought after for their crystal quality and locality significance. In spiritual traditions, garnet is traditionally associated with strength and grounding; these interpretations are cultural rather than scientific. From a mineralogical perspective, the appeal of this specimen lies in its calcium iron silicate composition, isometric symmetry, and formation within Morocco’s renowned mineral deposits. A genuine Andradite Garnet specimen from Khenifra Province, Tafilalet, Morocco, carefully chosen for quality and supplied with certificate of authenticity, offering impressive natural crystal form in a substantial 40–60mm size.
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