Trapiche emeralds are found in the black shale host rocks of just a few Colombian mines in the western belt of the Eastern Cordillera Basin. Their appearance consists of a central core, six arms and black shale dendrites – a crystalline, branching tree-like structure that forms between the arms and around the core.
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Trapiche emeralds are found in the black shale host rocks of just a few Colombian mines in the western belt of the Eastern Cordillera Basin. It has a central core, six arms and black schalled dendrites, a crystal-like tree structure, branching around the core between the arms. These are visible when the crystals are positioned perpendicular to the c-axis and are often cut like cabochons to accentuate the six partitions.
The radial pattern has a considerable variance, and often includes a hexagonal structure at the core. There is still no consensus on the mechanism by which the pattern is formed or the conditions required for it. Several models have been suggested. According to one view, the black impurities are the remains of the slate matrix in which the emeralds grew, stuck between the radial dendrites of the growing emerald. The trapiche pattern is not an asterisk, an optically similar pattern that forms in a different phase.
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Trapiche emerald is a rare variety of gemstone emeralds, distinguished by a six-point radial pattern of ray-like spokes of dark impurity. It is one of several types of trapiche or trapiche-like minerals, including trapiche ruby, sapphire, granate, chiastolite and tourmaline. The name comes from the Spanish word trapiche, a sugar mill, due to the resemblance of the pattern with the spokes of the grinding wheel.
Trapiche emeralds were first described by Émile Bertrand in 1879. They are generally only (and rarely) found in the western part of the Eastern Cordillera basin, in the Muzo, Coscuez and Peñas Blancas mines of Colombia (but likely not in Chivor as reported in older literature). Singular finds in Brazil and Madagascar have also been reported.
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