A 'mineraloid' is a
mineral-like substance that does not demonstrate crystallinity. Mineraloids possess chemical compositions that vary beyond the generally accepted ranges for specific minerals. For example,
obsidian is an
amorphous glass and not a
crystal.
Jet is a dense form of
coal.
Opal is another mineraloid because of its non-crystal nature.
Pearls, considered by some to be a mineral because of the presence of calcium carbonate crystals within their structure, would be better considered a mineraloid because the crystals are bonded by an organic material and there is no definite proportion of the components.
Common Mineraloids
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Amber, organic, non-crystal structure.
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Anthracite, a variety of coal, "hard coal."
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Coal, organic, nonhomogeneous, and non-crystal structure.
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Jet, not considered a true mineral due to organic, non-crystal nature, a mineraloid.
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Lignite, a variety of coal, "Brown coal."
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Limonite, amorphous hydrated iron oxide, a mineraloid.
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Obsidian, volcanic glass - non-crystal structure.
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Opal, non-crystal structure, a mineraloid.
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Pearl, often considered a mineral due to crystal components, but then not a mineral due to organic origin, probably should be a mineraloid.
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Petroleum, organic and liquid.
★ ''pyrobitumen'', organic, nonhomogeous, non-crystal structure.
★ ''Vulcanite'',
vulcanized natural or synthetic rubber, thus not a mineral due to organic composition, lack of crystal structure, and not naturally occurring.
See also
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List of minerals Mineraloids are listed after minerals in each alphabetically sorted section.