Quartz is a hard, crystalline mineral with a hexagonal crystal structure. It is often found in the form of prismatic crystals with six-sided terminations. Its color can vary, but it is commonly colorless or white. However, impurities can give quartz a wide range of colors, including pink, purple, yellow, and smoky brown.
Quartz forms in a variety of geological environments, including igneous, metamorphic, and sedimentary rocks. It can be found in hydrothermal veins, granitic pegmatites, and as a primary component of sandstone. Additionally, quartz is a common constituent of many types of mineral deposits.
Quartz has numerous practical uses due to its physical and chemical properties. Some common applications include:
Studying quartz provides insight into the Earth's geology and the diverse ways in which minerals contribute to everyday life. Its unique properties and widespread distribution make it a fascinating subject for scientific exploration.