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Marble Stone is a rock resulting from metamorphism of sedimentary
carbonate rocks, most commonly limestone or dolomite rock. Metamorphism
causes variable recrystallization of the original carbonate mineral
grains. The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals. Primary sedimentary textures and structures of the original carbonate rock (protolith) have typically been modified or destroyed. *Colour may vary from that shown |
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Quartz is the second-most-abundant mineral in the Earth's continental crust, after feldspar. There are many different varieties of quartz, several of which are semi-precious gemstones. Especially in Europe and the Middle East, varieties of quartz have been since antiquity the most commonly used minerals in the making of jewelry and hardstone carvings. *Colour may vary from that shown |
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