Almost all minerals consist of mixtures of compounds. A compound is a molecule or polyatomic structure containing more than one element; a mixture contains more than one type of molecule. Both must contain more than one atom, so they are not pure elements. Most minerals are in fact oxides, such as silica (silicon dioxide) or alumina (aluminium oxide).
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The most common mineral group contains silicate minerals.
Oxygen.
A mineral, or in most cases, a combination of minerals.
the most norenewable mineral is coal
The most common mineral group is the silicate mineral group, which is characterized by minerals containing silicon and oxygen, often combined with other elements such as aluminum, iron, calcium, or magnesium. Examples of silicate minerals include quartz, feldspar, and mica.
feldspar
Not necessarily. An ore is a mineral deposit that contains some resource that can be extracted profitably. So while ores are minerals, most minerals are not ores.
The most common mineral group is the silicate mineral group, which includes minerals such as quartz, feldspar, and mica. Silicate minerals are composed primarily of silicon and oxygen atoms, along with other elements like aluminum, potassium, or iron. They make up over 90% of the Earth's crust.
Quartz is the most abundant single mineral. Feldspars are, as a group, the most abundant minerals. Quartz and feldspars are classified as silicate minerals, the classification of mineral with the most abundance in the Earth's crust.
Some of the most useful physical properties of minerals include hardness (measured on the Mohs scale), cleavage and fracture (how a mineral breaks), color, streak (color of mineral powder), luster (appearance of a mineral's surface), and crystal habit (the shape in which a mineral naturally occurs). These properties help identify and classify minerals.
Most mineral ores are under the surface. Mining minerals can be profitable.