Formed by the recrystallization of pure sands under extreme heat and pressure, Fusion Quartzite personifies absolute resilience. Composed of 97% quartz, its white equigranular matrix offers a clean and sophisticated aesthetic. Its ultra-low porosity and superior hardness make it the premium choice for high-end countertops and flooring, ensuring that the beauty sculpted by nature remains immutable throughout time.
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.
A group of phyllosilicates known for their green color, from the Greek “chloros.” It is typical of low-grade metamorphic rocks like greenschist. It forms from the alteration of minerals rich in iron and magnesium. It looks like mica and flakes apart, but its layers are not elastic and won’t return to their original shape after being bent.
A fine-grained muscovite, rich in potassium and aluminum. It forms from the alteration of feldspars in hydrothermal zones and defines the foliation of metamorphic rocks. Its silk-like shine inspired the mineral’s name. Commonly found in schists, it helps indicate the intensity of geological changes in the Earth’s crust.
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