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Minerals are naturally occurring, inorganic substances with a defined chemical composition and crystalline structure. They are the building blocks of rocks and are found in a wide variety of environments, ranging from the Earth’s crust to deep within its mantle.
Minerals are classified based on their chemical composition and physical properties. There are over 5,000 known minerals, with new ones being discovered and named regularly. Some common mineral groups include silicates, carbonates, sulfides, oxides, and native elements.
Silicates are the most abundant mineral group and are composed of silicon and oxygen atoms, often combined with other elements like aluminum, iron, or magnesium. Quartz, feldspar, and mica are examples of silicate minerals.
Carbonates are minerals composed of carbon, oxygen, and other elements like calcium or magnesium. Calcite and dolomite are common carbonate minerals found in rocks like limestone and marble.
Sulfides are minerals containing sulfur combined with metals like lead, zinc, or copper. Galena and pyrite are examples of sulfide minerals.
Oxides are minerals composed of oxygen combined with metals like iron or titanium. Hematite and magnetite are common oxide minerals.
Native elements are minerals composed of a single element, such as gold, silver, or diamond.
Minerals play essential roles in various aspects of human life, from construction materials like granite and marble to industrial uses like iron ore for steel production. Additionally, minerals have cultural significance and are used in jewelry, art, and metaphysical practices. Understanding minerals is fundamental to fields like geology, mineralogy, and materials science, as they provide insights into the Earth’s history, processes, and resources.