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Grape chalcedony is a relatively recent discovery in the mineral market. The first specimens were found in 2016 on the Indonesian island of Sulawesi, specifically in the Manakarra area. Grape chalcedony is a variety of quartz and is characterized by distinctive spherical aggregates called spherulites, which form by precipitation from gelatinous solutions rich in silica (SiO₂). These spherical structures, often up to 1 cm in size, are composed of tightly packed, thin filaments of the same length. The individual spheres are often fused together or to the underlying rock, forming a cluster-like shape, hence the name. Grape chalcedonies are known for their delicate or intense colors, particularly purple and green. The purple color is caused by the presence of manganese, while the rarer green specimens get their color from other impurities in the rock. Specimens can also be covered in tiny quartz crystals, giving them a shiny appearance. They form during low-temperature hydrothermal processes in fractures and cavities in volcanic rocks. This process allows chalcedony to crystallize in typical botryoidal forms. Like all forms of quartz, grape chalcedony is highly mechanically and chemically resistant, making it a durable material suitable not only for collecting but also for creating jewelry such as pendants or earrings.
Grape Chalcedony – Sulawesi, Indonesia – 10pcs - HCH325
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HCH325
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