kvartskristalli
Kvartskristalli, also known as quartz crystals, are a common form of silicon dioxide (SiO2). They are characterized by their crystalline structure, typically forming hexagonal prisms terminated by pyramids. Quartz is one of the most abundant minerals in the Earth's crust, found in a wide variety of geological environments. Its formation can occur through igneous, metamorphic, and sedimentary processes. Pure quartz is colorless and transparent, but impurities can give it a wide range of colors, leading to varieties like amethyst (purple), citrine (yellow), rose quartz (pink), and smoky quartz (brownish-grey).
The physical properties of quartz, such as its hardness (7 on the Mohs scale), chemical inertness, and