silicate: feldspar and mica
non-silicate: halides and native gold
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An element that is a metal is more likely to give away its electrons because metals tend to lose electrons in chemical reactions to achieve a stable electron configuration. Sodium and potassium are common examples of metals that readily give away electrons.
A sheet-like silicate structure refers to a mineral arrangement where silicate tetrahedra are stacked in a sheet-like fashion. Examples include minerals like mica and clay minerals, where the tetrahedra are arranged in continuous flat layers. These structures give the minerals their characteristic properties, such as cleavage and low hardness.
Hot water is able to hold dissolved solids such as minerals. These minerals are thought to give hot springs their therapeutic properties.
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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).
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Some minerals include stuff you might have in your cereal like iron and zinc.
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Yeast, Sponge, and mold
Rose plant and Henna plant.
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