Minerals can be classified into 13 groups according to their constituents. The major groups are: (1) native elements; (2) sulfides; (3) sulfosalts; (4) oxides and hydroxides; (5) halides and borates; (6) carbonates; (7) nitrates and iodates; (8) phosphates, vanadates, and arsenates; (9) sulfates; (10) tungstates and molybdates; and (11) silicates.
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The two major groups of minerals are silicate minerals and non-silicate minerals. Silicate minerals are the most abundant and contain silicon and oxygen, while non-silicate minerals do not contain silicon and oxygen in their chemical composition. Silicate minerals make up over 90% of the Earth's crust, while non-silicate minerals include groups like carbonates, sulfates, halides, and oxides.
Minerals are divided into many more than two groups based on their chemical composition. The broadest divisions of the classification used in the present discussion are (1) native elements, (2) sulfides, (3) sulfosalts, (4) oxides and hydroxides, (5) halides, (6) carbonates, (7) nitrates, (8) borates, (9) sulfates, (10) phosphates, and (11) silicates.
•Two divisions-Major: Calcium, Sodium, Potassium, Chloride, Phosphorus, Magnesium, Sulfur-Trace: Selenium, fluoride, iron, chromium, manganese, iron, zinc, copper•Generally act as coenzymes for metabolic reactions
here are two kinds of minerals: metalic and non-metalic. metalic is made of metal, and non-metalic is not. the metalic characteristics are generally noticable. so putting it simply its either a metal or a rock
Silicate minerals are minerals that has a combination of silicon and oxygen. Non-silicate minerals are minerals that do not have a combination of silicon and oxygen.
They are divided into silicate and nonsilicate. I'm not sure if that's how you spell it though. Sorry if it's wrong! : )
The major groups of minerals are silicates (e.g., quartz and feldspar), carbonates (e.g., calcite and dolomite), sulfides (e.g., pyrite and galena), oxides (e.g., hematite and magnetite), and sulfates (e.g., gypsum and barite).
The two main families of rock forming minerals are silicate minerals and non-silicate minerals. Silicate minerals are the most abundant and include minerals such as quartz and feldspar, while non-silicate minerals include groups like carbonates and sulfates.
Nonmetallic mineral resources can be divided into two groups: industrial minerals (such as gypsum and salt) and building materials (such as sand, gravel, and limestone). Industrial minerals are used in various industries, while building materials are used in construction and infrastructure projects.
The two major components of soil are minerals (inorganic matter) and organic matter. Minerals come from the weathering of rocks and provide essential nutrients for plant growth, while organic matter is composed of decomposed plant and animal material that helps improve soil structure and fertility.
Renewable resources and non-renewable resources. Renewable resources can be replenished over time, such as sunlight and wind. Non-renewable resources are finite and will be depleted over time, like fossil fuels and minerals.