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Pyrope
8 in the gallery
Pyrope is a garnet mineral that forms as a nesosilicate, typically presenting a vivid red to purplish-red color and a glassy to vitreous luster. Crystals are commonly euhedral or prismatic, often displaying well-defined faces that reflect light with a bright, resinous sheen. The mineral's name is associated with its magnesium-rich composition within the garnet group, and it occurs in metamorphic and igneous rock environments where high temperature and pressure stabilize garnet minerals. Notable specimens historically originate from classic garnet provinces and high-temperature metamorphic zones, producing sharp crystals that are prized by collectors for their color and transparency.
- Formula
- Mg3Al2(SiO4)3
Where Pyrope is found
About Pyrope
Collectors prize Pyrope for its rich color, clarity, and the way crystals can form sizable, well-formed aggregates. Specimens from notable localities can showcase dramatic color zoning, sharp single crystals, or dramatic cubic-like or dodecahedral terminations that catch the eye in hand-held displays. While Pyrope occurs globally, high-quality material from traditional garnet-bearing terrains remains highly sought after for study and display, illustrating the mineral’s role in metamorphic petrology and its enduring appeal to mineral enthusiasts.
