Formed under massive tectonic pressure, Matrix Schist is a one-of-a-kind metamorphic stone. Its foliated structure, with quartz alternating with micas like biotite and muscovite, gives it a natural silver shimmer and a really distinctive feel. Every slab hints at the flowing motion of the Earth’s crust, giving architects an organic, modern look—perfect for cladding when you want depth, texture, and a refined geological vibe.
Every detail in natural stone comes from the perfect mix of minerals, creating colors, veins, and textures that can’t really be copied. It’s a natural formation that holds the story of the Earth, shaped over millions of years.
A very common mineral in the continental crust made of pure silica. It is essential in granites, sandstones, and quartzites and is known for its high hardness and glassy shine. It is highly resistant to weathering and forms beach sand. It comes in many colorful varieties, like amethyst, and is important for making glass and watches.
Biotite – rich in iron, magnesium, and potassium. It is commonly found in igneous rocks like granites and in metamorphic rocks like gneisses. Its perfect cleavage allows the mineral to peel into thin, flexible, and elastic sheets. Its dark color and glassy shine are very typical visual traits in rocks from the Earth’s crust.
The most common white mica in the Earth’s crust. It is rich in potassium and aluminum and is found in granites, pegmatites, and schists. It stands out for its perfect cleavage, allowing it to peel into thin, flexible, and transparent sheets. It was once used as glass in ancient Russia and today is used as a thermal and electrical insulator and in cosmetic shine products.
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