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Silicates are minerals that are composed of oxygen and silicon. These can be found in a variety of rocks and account for approximately 90% of the Earth's crust. Quartz, feldspar, and mica are some of the most prevalent silicates. Silicate is a tetrahedral network of SiO 4 4 ions with oxygen atoms at the vertices. A SiO 4 4 tetrahedron is formed by four oxygen atoms surrounding each silicon atom. Several silicate minerals, including quartz, feldspar, and olivine, have a silicate structure.

There are several forms of silica, the most prevalent of which being quartz and silicon dioxide. Sand is primarily composed of silicon dioxide, and quartz is the most prevalent form of quartz. Silicates minerals are a kind of minerals made up of silicon and oxygen and have the chemical formula SiO2. Two common silicate minerals are quartz and tridymite. Quartz is the most prevalent mineral on Earth and may be found in all sorts of rocks. Tridymite is a high-temperature mineral found exclusively in igneous rocks. Quartz and tridymite are both hard minerals with a glassy appearance.

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