Minerals can be identified through simple tests that
Minerals can be identified through simple tests that evaluate characteristics such as color, brightness, trace, hardness, cleavage and reaction with acids. Color, although observable, is of little use in identification, as a mineral can have different colors. The shine can be metallic or non-metallic, depending on the light reflection. The trace refers to the color of the powder left by the mineral when it scratches a surface. Hardness, measured by the Mohs scale, indicates resistance to scratching, with harder minerals scratching softer ones. Cleavage, a mineral exhibits cleavage when it breaks, under the action of a force, along well-defined plane surfaces. Reaction with acids refers to the ability of some minerals to react with acids, producing effervescence. For example, calcite reacts with acid, releasing bubbles of carbon dioxide.
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